42 THE WARMING OF THE INDIAN OCEAN. THE CANARY IN THE COAL MINE

CAUSE OF WARMING

In general the planet warms as surface pressure increases in low and mid latitudes.

The chain of causation runs like this: Increased surface pressure is associated with increased geopotential height, extra warmth in the atmospheric column and a consequent reduction in the quotient of moisture held in the very expansive ice crystal form. As cloud cover diminishes more solar radiation reaches the surface of the planet. When energy is absorbed by the ocean it is stored to depth and, by virtue of ocean currents, re-distributed, fortuitously warming those parts that receive little solar energy.

In contrast, when solar energy falls on land it is swiftly, in the main overnight, returned to the atmosphere. The warming of the atmosphere that is occasioned in northern summer, due to the extensive land masses of that hemisphere,  results in a global deficit of cloud cover in the middle of the year producing the annual maximum in planetary temperature when the Earth is furthest from the sun and solar irradiance 6% diminished by comparison with January.  It should be obvious (how did climate scientists miss this?) that the primary dynamic determining surface temperature is the temperature of the atmosphere in relation to the moisture that it contains.

REDISTRIBUTION

Please inspect the map below. The planetary winds drive ocean currents that mix cold waters from high latitudes and the ocean deep into the warm waters of the tropics. This is evident on the eastern margins of the oceans and particularly so in the southern hemisphere. The Indian Ocean is the odd man out with a weak cold current on its western margins and a warm, southward travelling, current on its eastern margin. The consequence is a relative backwater that is less  affected by the mixing of cold with warm water.

global-sst

It follows that the circulation of the oceans results in a very different thermal regime in each basin according to the  the ocean currents that are primarily driven by the winds. As the winds evolve, so do the currents.

The table below documents the extent of the temperature increase  over the last 68 years according to latitude and longitude in the three major ocean basins. For economy I focus on those latitudes that are warm enough to be relatively hospitable  to man.

sst-in-numbers

It is obvious that the bulk of the Pacific Ocean has not warmed to the same extent as the Indian and Atlantic Oceans. In terms of basin averages, in January the Indian Ocean has warmed by 0.87°C, The Pacific by 0.42°C and the Atlantic by 0.46°C. In July the Indian has warmed by 0.84°C the Pacific by 0.12°C and the Atlantic by 0.6°C. It is in July that the contrast between the oceans is strongest.It is the Indian Ocean that has warmed to the greatest extent.

THE SURFACE PRESSURE DYNAMIC

annual-slp

If we are to understand the differences in the rate of warming of the Ocean basins we need to comprehend to role of polar cyclones in high latitudes. Enhanced polar cyclone activity in the Antarctic circumpolar trough (red and orange in the map above) has, over the period of record, shifted atmospheric mass into low and mid latitudes from latitudes south of the 50° parallel. In consequence the high latitude west wind drift that is coextensive with the circumpolar trough, that drives cold water into the tropics, has accelerated. The flow is restricted at the Drake Passage between the Pacific and the Atlantic. Accordingly the Pacific Ocean cooled in parts and generally warmed at a much reduced rate when compared to the Indian and Atlantic Oceans.

drake-passage

The Indian Ocean is like the canary in the coalmine, a companion to the miner to warn him of a change in the quality of the air. The evolution of surface temperature in the Indian Ocean offers a glimpse of unfettered reality in terms of the march of surface temperature across the globe as it is forced by change in cloud cover associated with shifts in atmospheric mass and the change in the planetary winds.

The remainder of this chapter explores the shift in atmospheric mass from high southern latitudes and its relationship to surface pressure in the rest of the globe and the Indian Ocean in particular.

The discussion is is not based on the hypothetical constructs of a climate model or the abstruse mysteries of so called ‘planetary forcings’.  Rather it is grounded in observation and measurement based on data as  presented in the reanalysis work of Kalnay et al accessible here.

The graph below represents the evolution of surface pressure in the Indian Ocean south of the equator.We must to answer the question: Why is it so?

slp-indian-ocean-south-of-equator

WHY WORRY

The entire southern hemisphere has not warmed in the month of December in the last 68 years. If surface temperature were being forced by increased back radiation from the atmosphere the southern hemisphere should warm in all months.  There is no reason to expect the degree of warming due to a hypothetical increase in back radiation to be different in one month to another.  We therefore discard the hypothesis that temperature at the surface is driven by the carbon dioxide content of the atmosphere.  We look for other mechanisms to explain the flux in surface temperature. Radiation theory is all very well but in the real world, inoperable. The concept of anthropogenic warming is a distraction from fairyland. We can, to advantage, be more discriminating in what we choose to believe.

SURFACE PRESSURE DYNAMICS

sh-high-lat-surface-pressure
Figure 1 Sea level pressure in the region of the Antarctic circumpolar trough compared to sea level pressure in the entire region south of 50° south latitude.

Figure 1 compares the evolution of sea level atmospheric pressure in the Antarctic circumpolar trough to all latitudes south of 50° south. It is plain that the relatively short term fluctuations in surface pressure in the larger entity are greater than in the ‘trough’. In point of fact the trough expands and contracts across the parallels affecting surface pressure in adjacent latitudes and in particular across the Antarctic continent. The agent of change is polar cyclone activity that is energised by differences in atmospheric density between very different parcels of air that meet in the region of the trough in the very broad interface between the stratosphere and the troposphere between about 400 hPa and 50 hPa. It is in this region that the strongest winds are to be found. Polar cyclones are generated aloft. This is the nature of the ‘coupling of the troposphere with the stratosphere’, a concept that is a postulate of conventional climate science but remains a mystery so far as its modes of causation is concerned. If one is wedded to radiation theory it limits the mind.

slp-50-90-s-and-90n-to-50s
Figure 2 twelve month moving averages of sea level pressure either side of the 50° south latitude band encompassing the globe as a whole.

In figure 2 we compare the evolution of surface pressure south of the 50° south  parallel of latitude with surface pressure north of that same parallel. If the total mass of the atmosphere were to be invariable we would expect a strictly reciprocal relationship. As pressure falls on one side of the 50th parallel it should rise on the other. Plainly, the increase, decrease and subsequent increase in surface pressure in concert, between 1948 and 1964, is evidence of a planetary evolution in the quantum of atmospheric mass perhaps associated with enhanced loss in very active solar cycles and incremental gain in quiet cycles. That is a subject for another day.

Plainly, since 1964 it is the reciprocal transfer relationship that dominates. When atmospheric mass is lost south of the 50th parallel it moves north the 50th parallel and vice versa.This process of exchange is referred to as the Antarctic Oscillation.

slp-indian-versus-90n-50s
Figure 3

In figure 3 we compare the evolution of surface pressure in the Indian Ocean south of the equator through to 30°of latitude with that north of the 50th parallel.

indian-versus-90n-70-50s-two-axis
Figure 4

Figure 4 presents the same information as in figure 3 but on two axes with independent scales. It’s plain that broadly speaking the Indian Ocean south of the equator gains and loses atmospheric mass in parallel with all points north of the 50th south parallel but there are short term differences. These discrepancies are likely due to complex interactions between the southern and the northern hemispheres where, depending on the time of the year the Arctic Oscillation imposes change in the southern hemisphere or in the reverse, the Antarctic Oscillation imposes change on the northern hemisphere, tending to produce ‘mirror image’ results. Short term variations in these two data series  can be in opposite directions.

sst-indian

Figure 5

In figure 5 we compare the evolution of sea surface temperature in the Indian Ocean north of the equator  with that south of the equator.  The data is a twelve month moving average of monthly  means so as to remove the seasonal influence. It is plain that the more extreme variations occur north of the equator. Nevertheless the series are very similar in their evolution with generally coincident peaks.

sst-and-slp
Figure 6

In figure 6 we compare the evolution of sea level pressure in the Indian Ocean to the south of the equator with the evolution of sea surface temperature in the Indian Ocean north of the equator. Sea surface temperature tends to lag surface pressure by a few months. Plainly the Antarctic Oscillation affects sea surface temperature via coincident heating of the atmospheric column as reflected in increased geopotential height driving a reduction in cloud cover.

indian-ocean-sst-and-gph
Figure 7

Figure 7 looks at the relationship between geopotential height and sea surface temperature. Note that geopotential height is strongly related to sea surface temperature but the relationship is  not proportional. It is not the increase in sea surface temperature that drives the increase in geopotential height but warming of the air column due to the increase in the ozone content of the air within descending columns of air. These air columns reflect in their temperature the increased surface pressure, the increased warming at the surface and the increase in the ozone content of the descending air. At 200 hPa the air is warmer in winter than in summer due to enhanced ozone content in winter. The temperature of the air is independent of the temperature of the surface over which it lies.

slp-and-sst-monthly-indian
Figure 8 Sea level pressure in the Indian Ocean south of the equator compared to sea surface temperature north of the equator. Temperature lags pressure.by several months. There is pronounced warming in southern hemisphere winter months and occasional warming cycles in the summer months, notably in 2009-2010 and 2012- 2013. This warming is tied to the ozone content of the air in high latitudes.

In figure 8 we focus on monthly data.  Shown is the departure of a particular month’s data from the whole of period average for that month.

This graph reveals a climate system that is capable of swinging between a sea surface temperature anomaly of about -0.3°C and +1.2°C in an interval of between one and six years. The amplitude of this variation is almost double the increase in temperature that has occurred in the Indian Ocean over the last 68 years.  In this circumstance we should simply move on. There is nothing exceptional about this increase in temperature. There is no need to invoke new modes of causation to explain this phenomenon.

RECAP

Why has surface pressure and sea surface temperature in the Indian Ocean increased almost continuously since 2011? The answer lies in the forces that determine polar cyclone activity in the Antarctic circumpolar trough. Those circumstances relate to the  changing nature of the atmosphere in the area of overlap between the stratosphere and the troposphere in high southern latitudes.

As Gordon Dobson observed back in 1925, surface pressure is a by-product of total column ozone. Low pressure cells have more ozone aloft and exhibit a lower tropopause than high pressure cells.

Ultimately polar cyclone activity and surface temperature together with wind direction and intensity and the extent of mixing in the ocean  are a function of the ozone content of the air in high latitudes.

40 A WIND FROM THE SOUTH AND A WIND FROM THE NORTH

Ecclesiastes 1:6
The wind goeth toward the south, and turneth about unto the north; it whirleth about continually, and the wind returneth again according to his circuits.

This post revises key concepts that relate to the evolution of climate. Good teaching is about saying it again in slightly different ways until it sinks in. This caters for the students who can’t tune in at a particular time and many others whose perceptual frameworks are sort of ‘frozen’. Its also possible that the message can be delivered without the  necessary flair.

Knock-knock.  New idea. Fundamental to the nature of Earth is the difference between  the warmth of low latitudes and the cold of high latitudes.  Without the redistribution of energy by wind and water the extent of the habitable latitudes would be tiny. In the tropics there is little variation in the nature of the air from day to day. But in the mid and high latitudes change is the rule.  When the wind changes in a systematic fashion  to establish new states, we have climate change. The further we depart from the equator, the greater is the change that is experienced.

The air moves from zones of high to zones of low surface pressure. Pre-eminent in terms of low surface pressure is the Antarctic Circumpolar Trough. It is the zone coloured orange in figure 1.

Annual SLP
Figure 1

Kalnay et al’s reanalysis of 1996 to be found here. shows the evolution of surface pressure by latitude over time and is presented in a graphical format in figures 2 and 3.

July pressure
Figure 2.
January pressure
Figure 3

Plainly, the work that is done in redistributing energy across the latitudes is dependent on the evolution of surface pressure in the Antarctic Circumpolar trough and to a lesser extent the latitudes north of 50-60° north.

 

40-60-n-and-s-t-air
Figure 4

Figure 4 plots the temperature of the air as it evolved in the year 2015 at  500 hPa at 40-60° of latitude in the northern hemisphere at left and the southern at right. Plainly there is a north-west to south-east orientation in the movement of the air masses as  the atmosphere super-rotates about the Earth in the same direction that the Earth rotates, but faster. The speed of rotation increases in the southern hemisphere where the angle of attack is more aligned with the parallels of latitude. The air spirals from north to south at all latitudes.Warmer parcels will have an ascending  tendency while colder parcels will be descending.

THE IMPORTANCE OF POLAR CYCLONES

New Concept: It is polar cyclones that are responsible for the intensity and evolution of the circumpolar trough.

A core theme of this work is that Polar Cyclones are energised by warm, low density cores in that space where the troposphere overlaps with the stratosphere. Differences in the ozone content of the air gives rise to differences in air density. A chain of cyclones on the margins of Antarctica   give rise to a rapidly circulating polar vortex in the stratosphere. There are no limits to convection in the stratosphere.

In summer the air rises to the limits of the atmosphere directly over the continent of Antarctica but in winter there is descent. A rising cone of air surrounds the zone of descent. This cone is sometimes described as a polar vortex. The cone begins at 300 hPa over the circumpolar trough and widens to take in the mid latitudes at the highest levels.

The upper troposphere/Lower stratosphere in the region of the circumpolar trough is characterised by intense mixing of air from diverse origins, the troposphere, the stratosphere and the mesosphere.

Between October and March the cone of ascending air below 50 hPa tightens like a hangman’s noose bringing air from the troposphere to the pole, creating an ozone hole, the falling away of surface pressure at this time of the year associated with generalised ascent over the Antarctic continent and so excluding the flow of air from the mesosphere that descends throughout winter.

That the circumpolar trough is due to differences in the ozone content of the upper air should be non-controversial.

THE DENSITY OPACITY OF THE GREEN BLOB

The circumpolar trough is an unremarkable aspect of the atmosphere in the view of UNIPCC. The significance of its presence is  unappreciated. This is not an unusual state of affairs in the annals of humanity. In fact,  ‘Climate Science’ has not leaned a lot about atmospheric dynamics since the time of the pioneer Bjerknes who published a work on the near surface characteristics of polar cyclones in 1922.

Bjerknes

It is realised, at least in meteorological circles, that a trigger is required for the formation of low pressure cells of rotating air  in the region of the circumpolar trough. That trigger  is an upper level trough, a mass of warmer, low density ozone rich air.

In  1922 it was not apparent that the most vigorous winds are located in the overlap between the stratosphere and the troposphere. Neither was it apparent that cold ozone deficient air  from both the mesosphere and the tropical troposphere are drawn towards the circumpolar front in the space shared by the upper troposphere and the lower stratosphere.

In fact the concept of a ‘stratosphere’ was pretty new in 1922. In many respects we have not moved on from that position despite the passage of 100 years. Indeed much that was known prior to the 1970’s has since been forgotten in parallel with the increasing concern that man and the environment in which he lives are  incompatible entities. Educators went off in socially responsible directions. A fabulous gravy train  was created for scientists and space agencies and all those who aspire to gain their daily bread by looking after the environment, painstakingly monitoring the activities of a an every increasing panoply  of despoilers, at one end mighty global corporations and at the other the humble cow that provides the milk for your morning cereal irresponsibly farting in  its field of green. Such is the work of the modern missionary.

The intensification of polar cyclones in winter, and the consequent lower surface pressure at that time of the year is due to the proliferation of ozone. Gordon Dobson observed in the 1920’s that, in high and mid latitudes low surface pressure identifies areas with high total column ozone. Dobson measured wind velocity and discovered that the strongest winds were not at the surface but in the region of the tropopause. The tropopause is kilometres lower when surface pressure is low than when surface pressure is high. This circumstance may be described as an upper level ‘trough’, a zone of  reduced air density that shows up in elevated geopotential height contours. Had Bjerknes apprehended the structure of the upper air we would not now be worrying about carbon dioxide in the atmosphere. We would be aware that the source of long term climate change, the source of decadal variations, the source of inter-annual variations and indeed our daily weather lies in variations in the ozone content of the stratosphere. We would  be at peace with the notion that our ‘rather too cool for comfort’ planet gains and loses energy according to change in the extent of its cloud cover.

There is so much to learn.

 

38 UNCOMMON SENSE

Hemisphere surface temp
Fig. 1 Evolution of temperature at 1000 hPa in the Northern and Southern hemispheres of the Earth. DATA SOURCE:

According to Mark Twain, when it comes to numbers there are Lies, Damned Lies and Statistics.

Any form of manipulation to achieve simplification involves suppression of information.If one is to draw intelligent conclusions it is better to have all the original data. The less averaging the better.

Even the act of aggregating for a whole hemisphere, as is done in figure 1, is questionable. A sphere exhibits very different characteristics across its surface and so does  a half sphere. But, looked at in this way, its better to look at the two hemispheres seperately rather than together. The act of dividing the globe in half at the equator is a reasonable thing to do because the two are very different and we can learn in the process.

In figure 1  we have monthly data.  The peak in the cycle is the warmest month and the trough is the coolest month.Between the two are all the other months.

The two hemispheres are about as different as two planets. Temperature in the southern hemisphere (red line) exhibits a smaller annual range. Winter is marginally warmer than in the northern hemisphere. Summer is a lot cooler. In the Southern Hemisphere temperature is moderated by the extensive oceans.

In the Northern Hemisphere temperature is driven up due to the extensive areas of land. This  affects high more than low latitudes. The warming of the mid and high latitudes of the northern hemisphere in summer is due to atmospheric heating and loss of cloud cover. More solar radiation gets through the clouds to warm the surface. Paradoxically the Earth is furthest from the sun in July and accordingly solar radiation is 6% weaker by comparison with January. Straight away we see that atmospheric heating and cloud cover is the dominant influence on surface temperature while the degree of variation in surface very much depends on the ratio of sea to land. Who would have thought that? We have been told that it is the ‘greenhouse effect’ that makes surface temperatures what they are. In fact surface temperature depends on whether the Earths natural sunshade is in place or not and just how far a location is from the moderating influence of the sea. There is always less cloud over land than over the sea and particularly in those places where little rain falls.

In fact the ratio of land to water determines the extent of atmospheric warming and cloud cover on all time scales from daily through to annual. This is the strongest influence on surface temperature. Its due to the fact that the temperature of the air changes quickly and to a much greater extent than the amount of water vapour in the air that is required to form cloud. Water vapour content tends to be reduced by cold overnight temperatures giving us dew and cloud in the mornings and relatively clear sky at midday. The closer to the surface of the Earth, the more moisture can enter the atmosphere via evaporation from open water and plant transpiration. The more elevated the location, the colder is the air and , the lower is its moisture content. The higher the elevation, the less  the air is affected by warming and cooling at the surface. The higher the elevation the more the temperature of the air is determined by its ozone content.

When the ozone content of air increases and it warms via the interception of long wave radiation from the Earth, the response is measured as increased geopotential height. Surface temperature rises in proportion to geopotential height. That is due to the cloud cover response. Surface pressure, geopotential height and surface temperature all rise and fall together.This is the natural climate change dynamic driven by change in cloud cover.

Enough of these ramblings. Back to figure 1. The dotted lines in figure 1 are strictly horizontal. They have no slope. These lines assist the eye to  detect variations. There is a relatively small variability in temperature in the southern hemisphere in summer (upper limit of red series) over the last 69 years and no obvious trend. On this basis one can rule out carbon dioxide as a driver of surface temperature because the gas is well mixed. If there is a back radiation effect it needs to show its face here. Palpably it doesn’t. If the back radiation effect depends at all on enhancement by humid air and the presence of cloud we should see a continuous increase in the temperature of the air in the southern hemisphere from November through to March because this is the time of the year when cloud cover peaks. But, we see that there is no change in surface temperature in the warmest month of the year. However, we do see a gradual increase in coolest month temperature in the southern hemisphere from about 1970. This is the warming that needs to be explained.

Now, lets look at the northern hemisphere. Coolest month temperatures rise and fall over quite short time intervals. The 1970’s are the coolest decade in the northern hemisphere in terms of both the warmest summer month and the coolest winter month.   Northern Hemisphere temperature increased after 1998 in both coolest and warmest month and this too needs to be explained.

A QUESTION OF TIMING

The raw data doesn’t inform us as to whether the climate cooled or warmed in spring or autumn. Does that matter?  Come to think of it, if the global average rises due to an increase in temperature in the winter months is that really a problem. Would we not actually prefer warmer winters? Can we make rational decisions on the basis of a global average? Not really! Under a regime of dramatically increased summer temperatures with thousands dying of heat stroke and and dramatically reduced winter temperatures with thousands freezing to death, the average may be unchanged. We may think the planet is warming if we see a rising global average. But that could simply represent some warming in the coldest, abominably cold month so that month is slightly less abominably cold. Quoting the global average is the sort of thing that Mark Twain was complaining about.

Having dispensed with the CO2 furphy and the global average furphy we can now concentrate our on why the temperature changes as it does!

WHY HAS SURFACE TEMPERATURE CHANGED AS IT HAS

What stands out most in figure 1 is the warming that occurs in the southern hemisphere in winter (red line) starting in the 197o’s.

Given that the temperature of the air is a chilly 11°C in mid winter, this warming, and even more so, the warming of the northern hemisphere in winter, is unequivocally beneficial. This is a matter for congratulation rather than concern. We live in fortunate times. But it would be nice to know why this is happening because winter warming inflates the average for the globe as the whole and gives rise to a lot of hysterical  nonsense that is swallowed by an uncritical media that take the point of view that the science of climate is a matter for ‘scientists’ and the average global temperature  is Gods Word. These people have no idea what Mark Twain was talking about.

Politicians don’t read science. They read the daily papers. We get the blind leading the blind and a cabal of irresponsible scare mongers beating the drum and clashing the cymbals while snapping at the politicians heels demanding ‘clean energy’ and an end to ‘carbon pollution’. This is the modern ‘left’ in action. Its the Democratic Party in the US, the moneyed elite in the UK and an unholy alliance of Labour, The Greens and the soft underbelly of the Liberals in Australia. Even the Chinese, who in many ways are very practical people, seem to have fallen in love with this idea. If you muzzle the press, put the intellectuals in prison and rule with an iron fist you can do whatever you bloody well like. Can we pretend that what is happening in the West is somehow preferable? Can we point to a more rational and beneficial result from our ‘democratic process’? Cast not the first stone.

A PLAUSIBLE EXPLANATION

The warming of the northern hemisphere in both winter and summer starts in about 1998. Bear in mind that the warming in southern winter occurs at a time when global cloud cover plummets as the large land surfaces of the northern hemisphere heat the atmosphere. Is that warming  due to an increasing ozone content of the air and a consequent decline in cloud cover?

Figure 2 confirms a step up in temperature at the 10 hPa pressure level after 1976. This is predominantly a southern hemisphere phenomenon.  The step up occurs in winter.The consequent much enhanced feed of ozone into the  high pressure zones of descending air over the global oceans would reduce cloud cover. Under normal circumstances 90% of global cloud cover is to be found over the oceans and this is where high pressure cells form, especially in summer. When ozone rich air descends in a high pressure cell, the air warms (geopotential height increases) and this is always, without exception, associated with warming at the surface.So, the warming is due to loss of cloud cover.

Raw 10 hPa T poles
Fig. 2.  10 hPa temperature near the poles

Now, I want you to sanction something quite unorthodox and shocking.

In figure 2 the hand drawn line that links the high points in the summer maximum in the northern hemisphere is copied and applied to the northern minimum and to both the minimum and the maximum in the southern hemisphere. This unsophisticated ‘sleight of hand’ is performed as a ‘seeing aid’ to discern the points of difference. I guess I am just a frustrated artist and the mathematical exactitude of Excel is humanised by this process.I was once told by a plant breeder that if you cannot see the difference in plant performance by eye that difference is not worth measuring. It’s somehow comforting to realise that we don’t always need mathematical manipulations in order to get to the nub of the question.

Some points to note:

  1. Winter minimums are more variable than summer maximums and particularly so in the northern hemisphere.
  2. Whole of period change at 10 hPa  is greatest in the Antarctic. Those who make a close study of the matter have worked out that this is where natural climate change begins. Here is the documentation: Antarctica is the source of natural climate change.
  3. At the surface, the widest range in temperature between summer and winter is seen in the northern hemisphere but that is not the case at 10 hPa.  It is the southern hemisphere that exhibits the big variations.

Now in the last point we have an anachronism and a clue.  See Figure 3.

The wide range in temperature at 10 hPa in the southern hemisphere is due to the variable intake of mesospheric air over Antarctica in winter. This intake of cold air cools the upper stratosphere. It does not affect the temperature of the air at elevations below 300 hPa. The deepest cooling occurs at the 30 hPa pressure level in July.  Why is it so?

In winter surface pressure in the Antarctic region reaches a resounding planetary high. Nowhere else, anywhere on the globe, in any season of the year does surface pressure approach that achieved over Antarctica in winter. Air from the mesosphere has a low ozone content and it dilutes the ozone content of the atmosphere generally.The enhanced flow of mesospheric air into the southern hemisphere causes a generalised deficit in the ozone content of the air in the entire southern hemisphere. Alternatively, when the flow is choked off (surface pressure rises) there is an increase in the temperature of the air and its ozone content.

It is easy to see how the ozone content of the air can change over time via an alteration in the mesospheric flow.

Polar column temperatures

TEMPERATURE VARIABILITY

See figure 4 below. The short term variability that is seen in Arctic is much enhanced after February. It is initiated  by a fall in polar surface pressure signalled by a rise in the Arctic Oscillation Index (the two are inversely related). This increase in 10 hPa temperature  is likely reinforced in amplitude and duration by an increase in ozone partial pressure due to enhanced penetration of ionising cosmic rays as the stratosphere warms. The build up in the temperature over the polar cap is avalanche like in its suddenness. It represents the displacement of cold mesospheric air. The heating effect,  observed to last for weeks at a time, requires amplification to persist in this way. Otherwise it would be gone in ten days. Without amplification the descent of mesospheric air should re-establish in short order . Patently it does not.

T strat and AO 10hPa

Figure 4. Mean temperature at 10 hPa compared with the Arctic Oscillation Index.

In Fig. 2 we observe little difference between the hemispheres in the evolution of 10 hPa temperature in summer. There is a slight step up in 1976. And, the step up in summer is greater in the south than the north.The change in the ozone content of the atmosphere is global, affecting the entire year  and it is related to a fundamental change in the atmospheric circumstances over Antarctica, most pronounced in the winter season.

The ozone content of the air is rapidly propagated across the globe as we will see in figures 6 and 7 below. This testifies to the strength of horizontal winds in the stratosphere and most particularly in the area of overlap where stratosphere and troposphere occupy common ground.

So, the standout anomaly in figure 2 is the step change in 10 hPa temperature in southern winter after 1976. This step change in 10 hPa temperature is reflected  in surface pressure data in figure 5 below.

In fact this step change in 1976 is  reflected surface temperature data at every latitude across the entire globe as documented here.

SLP 75-90S

THE ACTIVE INGREDIENT:OZONE

As Gordon Dobson discovered in the 1920’s surface pressure  is a reflection of the ozone content of the air and vice versa. The fall in surface pressure at 75-90° south latitude documented in figure 5 is a direct consequence of the increase of the ozone content of the air. It is the ozone content of the air that affects its density, the weight of the entire column and hence surface pressure.

Wind strength in the atmosphere is intimately connected with the ozone content of the air. The air is relatively still near the surface of the planet and also at the highest elevations. Wind velocity is most enhanced in the overlap between the stratosphere and the troposphere between 300 hPa and 50 hPa where abrupt change in the height of the tropopause is associated with jet streams.

The 10 hPa level is virtually the top of the atmosphere because 99% of atmospheric mass is below that pressure level. The rapidly ascending circulation at the pole elevates ozone producing the greatest temperature response at the highest elevations as is evident in Fig 6. The strong temperature response at 10 hPa is due to convection of ozone rich air that increases ozone partial pressure at the highest elevations. That ozone mixes across the profile and affects the ozone content of the air in descending circulations in mid and low latitudes.

The pressure gradient (density differential) across the vortex in the upper troposphere/lower stratosphere where polar cyclones are initiated determines the strength of convection.  The density differential is increased seasonally as the ozone hole is established below 50 hPa when NOx rich air from the upper troposphere is drawn into the circulation over the polar cap during the final warming of the stratosphere.

The incidence of very much higher temperature at the 10 hPa pressure level after 1978 represents a step change in the fundamental parameters of the climate system.  There is not one climate system here but many, as many as there are days in the year. Changing the ozone content of the air in high latitudes alters surface pressure differentials and therefore it changes the planetary winds.

Temperature
Fig. 6

A QUESTION OF TIMING

In figure 7 below we chart the evolution of 10 hPa temperature  in selected months from the mid latitudes to the southern pole.

10 hPa T SH
Figure 7 The evolution of air temperature at the 10 hPa pressure level in high latitudes

10 hPa temperature over the pole is greater at 80-90° latitude than at lower latitudes in summer. This is when mesospheric air is excluded and ozone rich air gently ascends to the top of the atmosphere. This phenomenon occurs over Antarctica between October and February.

10 hPa temperature over the southern pole is inferior to that at lower latitudes when mesospheric air is drawn into the circulation between March and October.

After 1978 we see a change in the temperature profile in all months. This is particularly so from June through to November. The transition month for the final warming prior to 1978 was November. After 1978  the transition occurs  in October. Taken all-together this data indicates  a fundamental change in atmospheric dynamics that inevitably produces an increase in surface pressure, geopotential height and surface temperature in mid and low latitudes.

This is the source of the warming in southern winter. It has nothing to do with the works of man.

The change in the temperature of the air at the 10 hPa pressure surface in the Arctic is a product of the combined influence of atmospheric dynamics at both poles. The Arctic is  independently influential.  Its calling card is extreme temperature variability in January and February. This can be seen in Figure 1 in the surface temperature in the coolest months.

Climate change is a matter of observation and common sense. There is not much of it about. When it comes to numbers there are Lies, Damned Lies and Statistics. Undoubtedly the leading offender is the global average of surface temperature as disseminated by GISS, The NOAA  and the Hadley Centre, all dedicated to the dissemination of information in support of the nefarious activities of Global Green and the UNIPCC.

 

37 OZONE DRIVES ATMOSPHERIC DYNAMICS

In this post I give an account of the data provided in two papers from a group of authors who have described the the nature of the atmosphere and its dynamics in terms of its ozone content. The work creates a framework that advances our understanding of atmospheric processes and how they relate to external influences in an open system. In introducing the papers I provide an interpretation of atmospheric dynamics that goes beyond that of the authors and it will be best if readers go direct to the originals as a preliminary activity before reading what follows.

The Total Ozone Field Separated into Meteorological Regimes. Part I: Defining the Regimes ROBERT D. HUDSON, ALEXANDER D. FROLOV, MARCOS F. ANDRADE, AND MELANIE B. FOLLETTE  Published in 2003 and accessed here.

THE ABSTRACT

Traditionally, studies in the stratosphere using column ozone amount, ozone profiles, and dynamical variables at midlatitudes have centered on zonal averages of these quantities made over specific latitude bands. This is in sharp contrast to the studies made within the polar vortices where the average is made within regions defined by potential vorticity, a meteorological parameter. An analysis of the ozone field in the Northern Hemisphere outside of the polar vortex is presented in which it is shown that this field can also be separated into meteorological regimes. These regimes are defined as 1) the tropical regime, between the equator and the subtropical front; 2) the midlatitude regime, between the subtropical and polar fronts; 3) the polar regime, between the polar front and the polar vortex; and 4) the arctic regime, within the polar vortex. Within each regime the zonal daily mean total ozone value is relatively constant, with a clearly separate value for each regime. At the same time, the stratospheric ozone profiles are clearly distinguishable between regimes, each regime having a unique tropopause height. A midlatitude zonal average, whether of ozone profiles, total ozone, or dynamical variables, will depend on the relative mix of the respective values within each regime over the latitude range of the average. Because each regime has its own distinctive characteristic, these averages may not have physical significance.

Here is the  introduction to the work:

Dobson et al. (1927) reported ground-based measurements of the total column ozone using a spectrometer that observed the solar ultraviolet irradiance. They noted that when an upper-tropospheric front passed over the instrument, the total ozone value either dropped or rose sharply. Shalamyanskiy and Romanshkina (1980) and later Karol et al. (1987) divided ground-based total ozone measurements into three regions, separated by the polar and subtropical jet streams. They found that total ozone and temperature profiles had small variability within each region but changed sharply at the polar and subtropical fronts. The same change in ozone across a frontal boundary can be seen in the data from the Total Ozone Mapping Spectrometer (TOMS; McPeters et al. 1996).

Now, the authors don’t go on to say that the  jet streams at the fronts are a product of a contrast in air density in part due to the heating activity of ozone. They must give due respect to the school of climate science that sees the Earth as a closed system. If they took account of their own observation that, when moving from equator to Pole, the tropopause steps down in elevation at the subtropical front and again at the polar front where, on the polar side of the front there is no tropopause at all, thereby giving rise to severe gradients in atmospheric density then perhaps they might hypothesise that ozone is THE critical factor giving rise to jet streams, determining the weather patterns in the troposphere and the evolution of climate over time. But we must bear in mind that the climate establishment would punish them if they ventured that viewpoint. It is safer to leave the question open to interpretation. Those who would maintain that the distribution of ozone is a product of atmospheric dynamics in the lower troposphere and the chlorine content of the polar atmosphere due to the escape of chlorofluorocarbons into the atmosphere from refrigerants etc etc, can then interpret matters as they prefer.

In establishment climate science there is no concept of ozone variation on an inter annual basis due to the activity of the mesospheric vortex at the pole or ozone production due to cosmic radiation. The atmosphere is not an electromagnetic medium capable of change in its rate of rotation due to change in the solar wind. In the conventional viewpoint the temperature of the stratosphere is not driven by the absorption of long wave radiation from the Earth by ozone but by the interception of short wave radiation from the sun. In other words the direct impact of short wave radiation from the sun as held to be the reason for the temperature of the stratosphere even on the night side and regardless of latitude. The planetary winds are held to be driven according to the energy absorbed in near equatorial latitudes. Adherents don’t know how the atmosphere is shifted from high latitudes to low latitudes and wont be drawn to speculate on that matter at all. The blinkers are very firmly in place. Grant money and ones livelihood is at stake. Privately, one may admit in a whisper, that the Emperor has no clothes but publicly he is beautifully arrayed in the most impressive garments that money can buy.

In spite of these niceties some very useful analytical work has been done that establishes the distribution of ozone in relation to the position of the subtropical and polar fronts and there are big surprises that have very important implications in furthering our understanding of atmospheric dynamics..

Dist of ozone
Fig 1

In terms of atmospheric dynamics in the northern hemisphere we can note that the situation is different to that in the southern hemisphere. The circumpolar trough in surface atmospheric pressure surrounding Antarctica is so deep, and persistent across all seasons as to act as a global sink, conditioning the movement of the atmosphere globally. By contrast, in the northern hemisphere a trough of sorts develops in the north Pacific in winter associated with regional ascent of ozone rich air to the top of the atmospheric column while high surface pressure that is associated with the Antarctic continent in winter is associated with the Eurasian continent during winter, in the same latitude as the North Pacific low pressure zone.

It should be emphasised at the outset that the data in this study relates to a single day, the 11th March 1990. I will explore the importance of this choice by way of a postscript. In now way is the legitimacy or the conclusions of this study adversely affected by the fact that the data represents a single day. In fact, it is only by concentrating ones effort on single day that one can discern the dynamics at work.

Of immediate interest is that the stretched Mercator’s projection of Fig 1 involves spatial distortion. The fingers of low ozone content air interlaced with fingers of high ozone content air would look different  in a polar stereo-graphic view and they are strictly an artefact of the circulation on a particular day. The configuration of the northern hemisphere circulation is complex and ever changing due to the distribution of land and sea. If we were looking at the very much simpler circulation in the southern hemisphere it would be immediately apparent that air of tropical origin is drawn into a super-rotating west to east circulation with its highest rate of rotation at the polar vortex. The vortex is a feature of the stratosphere linked to an ascending circulation  via a chain of polar cyclones that entrain air from the troposphere, air from the stratosphere and air from the polar cap that has descended  from the mesosphere. The vorticity of these polar cyclones and the stratospheric vortex depends upon contrasts in air density between one side of the vortex and the other.Note the  location of the blue area (high ozone) and the green area (low ozone) in relation to the  vortex.  The authors locate the vortex  in  this way:  The solid red line marks the position of the sharp gradient in the isentropic potential vorticity (IPV) contours on the 450- K isentropic surface, which traditionally is assumed to mark the edge of the polar vortex”.  

The 450-K  isentropic surface lies between 70 mb and 50 mb pressure surfaces. This is at the altitude where ozone is in greatest abundance in the vertical profile. It is unequivocally in the stratosphere. It will therefore be the location where the ozone density gradient  is steeper than anywhere else in the vertical profile giving rise to very strong winds. Notice that there are two gaps in the the blue-black zone of highest ozone content These are areas of downdraught of low ozone content mesospheric air associated with the high pressure cells over land. One lies over East Asia and the other in the vicinity of Iceland. It is no accident that the vortex follows the junction of high ozone content warm air to the south and low ozone content cold air to the north. Unequivocally, elevated vorticity is linked to differences in air density linked to the origin of the air, its trace gas content, including ozone and NOx (not shown but  always present in air from the troposphere),  the formation of polar cyclones and therefore the flux in surface pressure between high latitudes and elsewhere that varies on all time scales. This flux in the pressure differential between high and mid latitudes is measured as the Arctic Oscillation and the Antarctic Oscillation.

What is described as the polar front in this work is likely a near surface phenomenon, the outer interface of a chain of polar cyclones that feed air into the Polar Vortex. The zone between the polar font and the polar vortex has very high ozone values. It is a zone of intense convection that is generated at the elevation of the Polar Vortex, propagating down to the surface where its troposphere manifestation is called a ‘cold core’ polar cyclone. No cyclone can develop with a cold core. The warm core is aloft where ozone captures outgoing radiation from the Earth.

TRANSITIONS AND UNEXPECTED HOMOGENEITY

Hudson et al notes in respect of the ozone data: The average for all of the data slowly increases with latitude until the polar vortex is reached. On the other hand, the average for the tropical, mid latitude, and polar regimes is relatively constant over a wide range of overlapping latitudes. There is also a clear difference between the average total ozone amounts for each of these regimes.

The transition zone between these dissimilar regions  is referred to as a ‘front’. The Polar Front only exists in the winter months when mesospheric air descends  to jet stream altitudes its rate of flow and integration with the wider atmosphere  contributing to the flux in the ozone content of the atmosphere generally. But this is not a  dynamic that is mentioned in this work. In summer there is no descent of mesospheric air and its disappearance is described as the final warming of the stratosphere after which the air over the polar cap gently ascends. In summer a  high ozone values over the Arctic  Ocean contribute to generalised ascent and the jet stream structures are fragmented.

Hudson et al reports that the fronts between different ozone regimes exhibit the same ozone content around the entire globe at any particular time. However the values are different according to the month of the year.See figure 3 below: In winter the fronts have higher ozone values than in summer. This emphasises the basic cell like structure and the homogeneity found within cells.

At the polar front the ozone value is highest in February. Readers of earlier chapters in this work will know that surface temperature variability between 30° south and 90° north latitude is greatest in January and February. There is a causal connection. The year to year variability in ozone partial pressure at the polar front is greatest in winter when ozone partial pressure is highest. In the transition from autumn to winter surface pressure over the Arctic rises strongly in November as the Antarctic releases atmospheric mass as the final warming in the stratosphere takes place. The increase in mass in the Arctic in November is reflected in the Arctic Oscillation Index (low values). In December, as ozone builds giving rise to active polar cyclones, surface pressure in high latitudes falls just as strongly as it has risen in the transition from autumn to winter. In this way, as Gordon Dobson observed, surface pressure is linked to the ozone content of the air. More importantly, as surface pressure falls in the Arctic a warm wind from the south finds its way further north bringing clement conditions. The zone of Ascent in the North Pacific develops strongly taking ozone to the top of the column. The  return circulation brings ozone into the high pressure cells of the mid latitudes, warming the air, increasing geopotential height, reducing cloud cover and increasing surface temperature.

These points are worth repeating. Gordon Dobson pointed out that ozone maps surface pressure with high ozone values corresponding to low surface pressure. Low pressure in the Arctic brings a flood of warm air from the south. Cool air is replaced by warm air. This is the Arctic Oscillation in action. In more recent terminology the AO is called the ‘Northern Annular mode’. It is not in the interest of the authors of this study to link ozone dynamics to change in surface temperature wrought by a change in the origin of the air. The notion that surface temperature is a response to the presence of carbon dioxide in the atmosphere has to be maintained if ones work is to appear in academic journals like ‘Science’ although the newly appointed editor of Science is reported to be saying that ‘science’ has lost integrity in the process of suppressing competing viewpoints. See here where it is reported that:  “Science editor-in-chief sounds alarm over falling public trust. Jeremy Berg warns scientists are straying into policy commentator roles.” Are the publishers of ‘Science’ reacting to falling circulation related to negative reader response? If so, this will be good for small ‘s’ science.

EVOLUTION OF OZONE PARTIAL PRESSURE AT THE FRONTS

Ozone values at the fronts
Fig 2. Evolution of ozone partial pressure at the subtropical and polar fronts. Readers should be aware that the front referred to is in the upper air, not at the surface. The material expression of the front is a change in the height of the tropopause so that warm ozone rich air is found adjacent to cold ozone deficient air.

It is  very interesting that the authors report that the ozone content of the air in the ‘Midlatitude Regime’ is invariable around the globe regardless of latitude or longitude. Apparently atmospheric mixing processes maintain this homogeneous state. This reinforces the long held view of a cellular structure in the atmosphere between the fronts. Inferentially, it supports the notion that elevated ozone in the ‘Midlatitude Regime’ is a product of in-situ ionisation of the polar atmosphere by cosmic rays during the polar night rather than transport from the tropics where the ozone content of the air is inferior. If one conceives the situation in this way  it is  obvious that the ozone content of the air in high and mid latitudes is driven by forces that are external to the system via polar dynamics rather than the interaction of short wave radiation with the atmosphere. The stratosphere warms in the winter hemisphere in the mid latitudes, obviously unrelated to the incidence of short wave radiation. This accentuates density differences across the fronts driving enhanced vorticity. External forces are capable of mediating the strength of the zonal wind in an electromagnetic medium such as the atmosphere, mediating the penetration of mesospheric air and the penetration of cosmic rays that very much depends on air temperature and density. Due to ionisation by cosmic rays it is possible for the synthesis of ozone to occur in the absence of short wave solar radiation.

EXTREME OZONE GRADIENTS, TROPOPAUSE STEPS, JET STREAMS ARE ALL LOCATED AT THE FRONTS

Hudson notes that using aircraft to measure ozone partial pressure  both Shapiro et al. (1987), and Uccellini et al. (1985), found a strong coincidence between large gradients in the total ozone measurements from TOMS and the position of upper-level jet streams, the frontal zones and  tropopause ‘foldings’ where there is a step up in the height of the tropopause.

Ozone field TOMS
Figure 3 Differentiation of the Polar, Midlatitude and Tropical Regimes
Rawinsonde profiles
Figure 4 Temperature profiles in the three regimes. Note that there is a step up in the temperature of the tropopause in moving from the tropical to the polar regime. Note the very different heights of the tropopause across the three regimes Bear in mind the impact on the atmosphere of the circulation that brings mid latitude and tropical air  to the poles to be mixed  and elevated per medium of polar cyclones and the stratospheric vortex.

Note the difference in the height of the tropopause across the three regimes for North America.on 11th March with Tropical (250 hPa), Midlatitude (300hPa) and Polar (400 hPa)   The fronts between these regimes consequently exhibit steps. At these steps marked differences in air temperature and density manifest in the horizontal plane. This is an unstable situation. From figure 4 (Hudsons Fig 9)  we see that in the tropical regime, the temperature of the air at the tropopause is -70°C, in the Midlatitude zone it is-60°C and in the Polar regime -50°C. In this circumstance, at the vortex, because temperature reflects density,  the vertical interval between 400 hPa and 300 hPa, a distance of some 2 kilometres will be marked by continuous upwards displacement of low density air  and as a result this displaced air will circulate about the globe as an ascending jet on the margins of the tongue of cold dense mesospheric air with occasional discontinuities (as noted above in relation to east Asia and Greenland) that will be marked by extreme turbulence. As this air ascends it must be replaced from below drawing in ozone rich, low density air from lower latitudes together with NOx rich air from the troposphere and some air from the region of the polar cap that is derived from the mesosphere via subsidence.

WHERE DOES THE ENERGY COME FROM TO DRIVE THIS SYSTEM

The energy is supplied via the Earth itself in the form of infrared radiation at twenty times the wave length of the energy originally derived from the sun. The agency for its transmission to the atmosphere is ozone that imparts energy with an efficiency that varies directly with surface pressure. It is here, at the polar vortex that the system exhibits the river of energy thus acquired, not in the tropics where the air is quiescent. The ascent does not respect a ‘tropopause’ because it goes to the top of the atmosphere giving rise to localised ozone ‘hot spots’ at 1 hPa.  These hot spots are likely found over the warmest part of the oceans in mid to high latitudes. When inspecting the temperature response in the upper stratosphere we see that temperature volatility increases with altitude, particularly above 30 hPa.

The system continuously elevates ozone to the top of the atmosphere from where it must return within the  Midlatitude cell. If there is appreciable loss of ozone via ionisation or chemical erosion in the upper upper levels of the Midlatitude cell there must be sufficient ozone created to  remedy the loss and so provide the means to energise the system on a continuous basis, day and night. The Earth obliges in terms of the energy requirement. But where does the ozone come from to replace that lost to chemical depletion and destruction by short wave energy from the sun?

A seasonal low in the incidence of short wave radiation from the sun means that the ozone necessary to sustain this system is not available from the solar source in the winter hemisphere. It’s unlikely that the requisite ozone could be sourced from the  subtropical zone in the summer hemisphere that is remote, across the equator where in any case ozone partial pressure is quite low and always so. So much for the Brewer Dobson Hypothesis! There is however another source of ionisation via cosmic rays.

Vert profile Arctic
Fig 5 illustrating the marked warming of the stratosphere in January and February bucking the winter cooling trend that manifests strongly after November, but very unevenly from year to year.

The waxing and waning of the polar jet stream will reflect atmospheric dynamics due to the changing ozone content of the air, inducing changes in density gradients  across the polar front that in turn affects the rate of intake of mesospheric air. Ionisation by cosmic rays depends upon air temperature almost certainly generating an ozone production dynamic that will amplify change according to the activity of the sun. These interactions affect vortex and polar cyclone activity that vary from week to week, year to year and across the decades according to the incidence of solar activity. Note the incidence of stratospheric ‘warmings’ in figure 5 from January through to April during which the muon count from cosmic ray activity, as measured at the surface and in ice cores is known to respond directly to the changing temperature of the stratosphere. The muon count is a direct proxy for the incidence of cosmic rays and indirectly a proxy for solar activity. See here for background or here for a lecture presentation.

INCIDENCE OF CHANGE IN THE CHARACTER OF THE AIR BETWEEN 400 HPA AND 40 HPA.

Ozonesonde profiles March
Fig 6 Ozone profiles. Note the variation in ozone content and the elevations at which these variations occur, an excellent indication  of the extent of ‘wandering’ across the latitude bands that is characteristic of  the fronts between regimes. When this ‘wandering’ is viewed from the perspective of a person on the ground, the passage of a front is perceived as a change in the origin of the upper winds that are either  cold and ozone poor, coming from low latitudes or ozone rich and warm when the upper air arrives from high latitudes. The change  in the upper air is accompanied by a change in surface air pressure

From figure 6 (Hudson 10) we can infer that the degree of variability in the source and ozone content of the air in the upper troposphere/lower stratosphere increases from the equator to the pole and is most marked in the polar regime that only manifests in winter.  We see that the largest variations in ozone partial pressure in the North American polar regime manifest between 400 hPa and 40 hPa. This interval carries 36% of the  mass of the atmospheric column. Because ozone maps surface pressure and it produces the lowest surface pressures in high latitudes this guarantees that the atmosphere must move from the equator towards the poles. Om the southern hemisphere this movement occurs in a gentle spiral with the air coming from west north west to east south east. Such is the strength of the Antarctic circumpolar vortex that the direction of movement is the same in the northern hemisphere. The vertical intervals where this movement is strongest can be inferred from fig 6. The region between 400 hPa and 40 hPa encompasses the upper troposphere and the lower stratosphere. That this region sees the greatest mobility has implications for the ozone content of the air over the polar cap when the final warming of the stratosphere occurs and mesospheric air is replaced by troposphere air rich in NOx giving rise to an ‘ozone hole’ and so ending the period where the Polar Front is in existence. This circumstance was not appreciated at the time when environmental activists succeeded in having many nations subscribe to the Montreal Protocol to limit emissions of certain halogens supposedly responsible for the ozone deficit. The dynamics behind the creation of the celebrated Ozone Hole are a mystery to climate science to this day.

ORIGIN OF THE DRIVER OF THE GLOBAL CIRCULATION

The surface pressure differential between low and high latitudes directly governs the circulation of the air near the surface and to first order determines the equator to pole temperature gradient. In addition, minor change in the ozone content of the air in the tropical and mid latitudes will drive change in geopotential height at all elevations and with it cloud cover and surface temperature. It should be born in mind that the circulation of the air at the 10 hPa level is equator-wards rather than pole-wards. Accordingly, ozone descends from the top of the atmosphere in mid and low latitudes within high pressure cells.Apart from the surface temperature effect due to change in the origin of the surface winds, the variability in the ozone content of the air in mid and low latitudes drives  a  change in cloud cover to further amplify the temperature effect due to the change in the origin of the wind. These are the central dynamics behind climate change on week to week through to inter-centennial time scales. Surface temperature varies directly with surface pressure and geopotential height. This is the nature of climate change.

The natural variation in sea surface temperature in the southern hemisphere is seen in Figure 7. In terms of causation that figure is instructive.

SH SST
Figure 7 Sea surface temperature in the southern hemisphere according to the Kalnay reconstruction.

Climate change in the southern hemisphere, considered as an entity, measured in terms of sea surface temperature, is largely a matter of temperature change in the winter months. The hemisphere is no warmer in December in the latest decade than it was seven decades ago. An inference as to the origins of climate change is not hard to draw. There is no room here to infer an anthropogenic effect via back radiation.

 

Temp and ozone dist
Fig  8 Ozone and the temperature of the air. Note the higher tropopause is in low latitudes where convection and NOx sculpts the ozone content of the air giving rise to a marked deficiency in ozone below 50 hPa by comparison withe mid and low latitudes. That is why the tropopause in low latitudes is as cold as the mesosphere over the poles and distinctly colder than the tropopause in the mid or high latitudes.

The relationship between the ozone content of the air and its temperature is provided in figure 8 ( Hudson 11). The lack of a 1/1 correspondence between the ozone content of the air and its temperature, given that ozone is an absorber of long wave radiation from the Earth and that this activity is the primarily cause for the unexpected warmth of the stratosphere, is due to the marked flux in the direction of the movement of the air in the stratosphere with warmer air of polar origin that has a lower temperature but a higher ozone content tending to move towards the equator above the 50 hPa pressure level while cold ozone deficient air from the mid latitudes and the tropics moves pole-wards between  the 400 hPa and 40 hPa pressure levels. The latter produces tongues of cold, relatively ozone deficient air showing up in daily and weekly data but obliterated in averaged data over longer time intervals. This phenomenon is reflected in figure 10 as a higher standard deviation in the partial pressure of ozone  between 400 hPa and 40 hPa in the mid latitude and polar regimes. This marked variability due to the origin of the air finds its ultimate expression in the Antarctic ozone hole that manifests below 50 hPa at the time of the final warming of the upper air in spring. Its absence in the northern hemisphere is due to the configuration of land and sea.

The acute reader will realise that there is no room in this circulatory regime for the Brewer Dobson  hypothesis generated in the 1950’s as a possible explanation for the elevated ozone content of the air in high latitudes. The air below 40 hPa moves in the direction of Antarctica or to the Arctic and is generally ozone deficient. The air above 40 hPa comprising just 4% of the atmospheric mass, moves equator-wards and as it does so is increasingly subject to ionisation of ozone by ultraviolet B from the sun.

THE FLUX IN OZONE ACROSS THE SEASONS

Average and STd Devn of TC ozone
Fig 9

Mean total ozone in Dobson units exhibits a different pattern of seasonality in each regime as seen in Fig 9, (Hudson’s figure 13).

Variability in total ozone in the tropics peaks in January and February with a subsidiary  volatility emanating from the Antarctic from August through to December that is associated with final warming dynamics.

Mid latitude and tropical regimes in both hemispheres exhibit strong variability in  northern winter driven from the Arctic. This translates directly to variability in surface temperature. This is natural climate change in action driven by the ozone content of the air in the upper troposphere and lower stratosphere. As noted above it operates by changing the origin of the wind and the extent of the Earths natural umbrella, cloud cover that on average shields 70% of the surface of the earth, less in northern summer and more in northern winter. Accordingly the greater amount of cloud is present when the Earth is closest to the sun in January and the greatest variability in surface temperature across the most of the surface of the earth including the all important southern oceans also occurs in that month. It is no accident that the Pacific Ocean tends to exhibit its largest swings in temperature in January and that marked variability in surface temperature in January  can be discerned in temperature data even in high southern latitudes.

The Arctic Polar regime shows a strong maximum and peak standard deviation in the middle of winter but also a marked amount of variability driven from Antarctica in northern autumn / southern spring at the time when surface pressure falls to its annual minimum at 60-70° south latitude. This is where polar cyclones  are generated on the margins of Antarctica and is the location of the absolutely dominant southern vortex..

CHANGE OVER TIME AND THE MANNER OF CHANGE

There is a second paper from these authors to be found here.:

The total ozone field separated into meteorological regimes – Part II: Northern Hemisphere mid-latitude total ozone trends R. D. Hudson1 , M. F. Andrade2 , M. B. Follette1 , and A. D. Frolov3  Published 2006.

ABSTRACT

Previous studies have presented clear evidence that the Northern Hemisphere total ozone field can be separated into distinct regimes (tropical, midlatitude, polar, and arctic) the boundaries of which are associated with the subtropical and polar upper troposphere fronts, and in the winter, the polar vortex. This paper presents a study of total ozone variability within these regimes, from 1979–2003, using data from the TOMS instruments. The change in ozone within each regime for the period January 1979–May 1991, a period of rapid total ozone change, was studied in detail. Previous studies had observed a zonal linear trend of −3.15% per decade for the latitude band 25°–60° N. When the ozone field is separated by regime, linear trends of −1.4%, 2.3%, and 3.0%, per decade for the tropical, midlatitude, and polar regimes, respectively, are observed. The changes in the relative areas of the regimes were also derived from the ozone data. The relative area of the polar regime decreased by about 20%; the tropical regime increased by about 10% over this period. No significant change was detected for the midlatitude regime. From the trends in the relative area and total ozone it is deduced that 35% of the trend between 25◦ and 60◦ N, from January 1979–May 1991 is due to movement of the upper troposphere fronts. The changes in the relative areas can be associated with a change in the mean latitude of the subtropical and polar fronts within the latitude interval 25◦ to 60◦ N. Over the period from January 1979 to May 1991, both fronts moved northward by 1.1±0.2 degrees per decade. Over the entire period of the study, 1979–2003, the subtropical front moved northward at a rate of 1.1±0.1 degrees per decade, while the polar front moved by 0.5±0.1 degrees per decade.

The subtropical and polar fronts are associated with the subtropical and polar jet streams, and have mean latitudes of about 30° and 60° N, respectively

The positions of the subtropical and polar fronts defined in Hudson et al. (2003) vary on a daily basis as the Rossby waves meander about their mean latitudes. These fronts  are not be confused with the cold and warm fronts associated with cyclonic flow close to the surface.

Note that: When the ozone field is separated by regime, linear trends of −1.4%, 2.3%, and 3.0%, per decade for the tropical, midlatitude, and polar regimes, respectively, are observed.  It is not possible that a linear trend of 3% per decade could be driven from the tropical regime where the trend is -1.4% per decade. To achieve this disparity the ozone trend has to be independently created in high latitudes, and likely more from one pole than the other. It is in fact the Antarctic that drives the multi-decadal and inter-centennial trend.

The authors note that: Between January 1979 and May 1991, the relative area of the Polar regime decreased by about 20%, while that of the Tropical regime increased by about 10%. There was no significant change in the relative area of the Midlatitude regime over this time period. These changes imply a net poleward movement of the subtropical and polar upper-troposphere fronts. That in itself warms the surface.

The fronts define the extent of the hemisphere occupied by masses of air of different temperature.  If the  northern hemsiphere fronts move north the hemisphere warms. The northward migration of the subtropical front implies an expansion of the relatively cloud free area and an increase in the energy absorbed by the oceans.

In this way, change in the ozone content of the air brings about a change in the surface temperature and the energy circulating within the Earth system. When one looks at the data as seen here, this mode of change is entirely consistent with the pattern of temperature change observed between 1948 and the present time.

CONCLUSION

The manner in which the top down generation of surface weather occurs, from stratosphere to troposphere, has been a matter of debate for almost twenty years in connection with what has been described as the ‘annular mode phenomenon’. The papers reviewed in this post are amongst the more significant works published in the field of climate science since the work of Gordon Dobson who devoted his life to the measurement of total column ozone. If we are to be critical, the shortcoming lies in failing to look at the historical record over a longer time interval, to examine the situation in the southern hemisphere and to speculate about mechanisms responsible for change. Simple questions like ‘Why is it so? and ‘What does this mean for the evolution of surface temperature?’ are of the greatest importance but it is precisely in this area that the politics of climate change get in the way.  Accordingly, the link between ozone and the formation of polar cyclones that relates to the evolution of surface pressure in high latitudes is not made. Nevertheless these papers ably support the most cogent explanation of the manner in which natural variations in weather and climate can occur on week to week through to centennial time scales.

Unfortunately, climate scientists are off with the fairies with their CO2 forcing hypothesis and show no sign of a desire to  research the manner in which the climate of the Earth responds to external influences. Work that suggests that the climate system is subject to external forcing is simply ignored… much to the detriment of humanity.

Postscript.

Variability in the distribution of ozone is a  feature of the northern hemisphere as the following diagrams reveal.

2014 850 hPa
Centres of polar cyclone development associated with elevated ozone content in the air.

 

2014 ozone
The circulation is moving west to east entraining ozone from centres of accumulation .

 

2014 N2O
N2O in trace quantities is associated descending air from the mesosphere that is largely devoid of ozone.

 

2014 500 hPa
Surface pressure and circulation of the air at 500 hPa
2014 1 hPa ozone
Accumulation of ozone over the north American continent at 1 hPa as a result of convection.
2015 TC
On 11th March 2015 the ozone concentrations are more dispersed.
2015 50 hPa Ozone
At 50 hPa the core of the circulation over the Arctic is relatively deficient in ozone
2015 50 hPa Ozone
At 50 hPa trace quantities of N2O are associated with air from the mesosphere and an ozone deficit. A wide band over the Eurasian continent also shows evidence of descent.
11th March 2016 TCO
On 11th March 2016 total column ozone is much enhanced over the Arctic Ocean and to a lesser extent over the north Pacific.

11 Mar 2016 50

At 50 hPa there is an ozone deficiency over the Eurasian continent.

At 50 hPa the distribution of ozone is similar with some contraction over the north Pacific and a clearer definition of the ozone deficient zone over the Eurasian continent.

2016 N2O
The ozone deficiency over the Antarctic continent is associated with low N2O content mesospheric air.

The circulation of the air in the stratosphere is about an elongated core of high surface pressure located over the Eurasian continent stretching from Scotland to Mongolia. Within this cell very cold air that has little ozone but tracers of N2O descends from the mesosphere. N2O is primarily derived from soils due to organic decomposition. It is abundant in low latitudes where it scalps ozone to produce an elevated tropopause.

20160311 SLP
An elongated band of high surface pressure is associated with the descent of mesospheric air entering the circulation tangentially.

 

20160311 10hPa
Mesospheric air enters the elongated core of a fast moving descending circulation at 10 hPa. At left is an ascending circulation that is rich in ozone.
2016-03-11 1 hPa ozone
The ascending circulation produces an ozone hot spot at 1 hPa. The descending circulation is associated with low ozone values at 1 hPa. In fact ozone rich air is spilling into this descending circulation changing its character as it descends. Pressure from short wave ionising radiation from the sun in high northern latitudes in March, at which time the sun is over the equator  will deplete  ozone at 1 hPa. The question arises: Where does the ozone come from that is required to energise this circulation?

 

 

 

35 CAPE LEEUWIN AS A PROXY FOR CLIMATE CHANGE

Matthew Flinders named Cape Leeuwin after the first known ship to have visited the area, the Leeuwin (“Lioness”), a Dutch vessel that charted some of the coastline in 1622. There are three Capes in the southern hemisphere that offer a landfall to sailors who take advantage of the westerly winds at this latitude.

Cape Leeuwin is surrounded by blue/green water. Its a long stretch from Cape Town to the south west corner of Australia and an even longer stretch to Cape Horn. There is very little land between 30° south and 70° south latitude. The wind blows vigorously from the west. When you gaze out to sea and and find yourself reaching for more clothing it is because the air is very fresh, it has the same temperature as a vast stretch of ocean.

This Ocean  is the Earths battery. It is the chief and only means of storing energy from the sun. Whatever energy gets through the cloud layer penetrates deeply into the water and is given up slowly. The ocean warms and cools in the same way that it develops a long swell on its surface. When riding across the swell you rise up slowly and fall down just as slowly regardless of the surface chop. If we are looking for ocean, the location of the Earths energy store, you find it here. It is for this reason that Cape Leeuwin lighthouse is a good proxy for what is happening to the globe as a whole.

If a steady 33 mph (30 knots) wind blows for 24 hours over a fetch of 340 miles there is a 5% chance of encountering a single wave higher than 35 ft (11 m) among every 200 waves that pass in about 30 minutes. At the latitude of Cape Leeuwin a 50 knot wind is frequently encountered. No trees can grow in the vicinity of the lighthouse, just grass and low scrub. There is a layer of salt on everything.

If one looks for consistent high variability in the temperature of the surface of the sea it is here, in the southern hemisphere that one finds it, and at the equator. Here the variability is due to change in cloud cover and the direction of the wind. At the equator there is little cloud, little wind but a big variation in the in-feed of cold water from high latitudes according to the speed of the ocean circulation that is driven by wind and wave in high southern latitudes. It is in high southern latitudes that one finds the strongest wind belts on the planet, the roaring Forties, the Furious Fifties and the Screaming sixties.

Lighthouse

Lighthouse and houses

The lighthouse at Cape Leeuwin dates from 1910 and so does the temperature record. A sample from 1915 to 1921 is presented below. There is a tiny diurnal and annual range  but strong cycles of warming and cooling. The daily range increases strongly in summer when hot winds from the continent tend to arrive on a ten day cycle associated with the passage of anticyclones. In winter, these winds off the land can be cold suppressing the maximum and reducing the diurnal range. There is considerable variability in the daily minimums in winter within and between years. Winter is the time of the year when the Antarctic dynamic associated with the ozone content of the polar atmosphere causes marked swings in the relationship between surface pressure in the mid latitudes and the Antarctic circumpolar trough affecting the rate of flow of the westerlies and at times bringing cold southerly wind from Antarctica. Frontal rainfall falls in winter. Summers are arid as cyclones  track well south. Autumn is a season of quiet air, and infrequent light showers when farmers clear up land for pasture and burn the native vegetation to reduce the risk of fire. With solid winter rainfall and deep soils the countryside supports the growth of large eucalyptus trees that drop leaves and twigs in summer, a worrying fire hazard but an essential store of nutrient for soil microflora and plants, tending to keep the soil cool and moist in the dry summers experienced on the western sides of the continents at this latitude. Not far away is a very large desert.

Swinger
Fig 1

The red ellipses in figure 1 are intended to take your eye to features of interest, in particular the shape of the variability in the curve when temperature is least and the extreme variability in the daily maximum in the height of summer.

Plainly, the climate is like the road that curls through the Karri forest as seen below.

Boranup

There is a conclusion that can be drawn from the data presented below: Between 1910 and 1992 the minimum daily temperature does not change. Between 1992 and 2015 it warmed slightly then cooled again, then warmed for about six years and cooled for another six and looks as if it will get back to the 1910 average of about 14.3°C in a few years time.

Straight up this tells us that either, there is no greenhouse effect due to carbon dioxide in the atmosphere or that some local influence is maintaining the status quo as the rest of the globe is warming. I believe that there is no greenhouse effect. I do know that there is a local factor enabling this place to retain the status quo as surface temperature increases elsewhere. Until we understand the latter influences we will not be free of fear of the former.

Carbon dioxide is plant food and it is greening the Earth and in particular the arid zones because a plant that is not starving for carbon dioxide does not have to open its breathing apparatus (stomata) as wide as an opera singer and it loses less moisture to evaporation in the process of acquiring its plant food. For godssake, plants are at the base of the food chain. We have the wherewithal to feed double the current population of the globe and yet global economies are in complete disarray, interest rates are negative, governments are printing money, nobody wants to invest,  commodity markets are reeling and the whole system is teetering on the edge of an abyss.  Something is very wrong in the way that we are ordering society. That something has a lot to do with climate scares.

In any case 14°C is too cool to support plant life properly. Photosynthesis is optimal at 25°C. The globe is too cold for comfort, too cold to support photosynthesis over the bulk of its area for too long in the annual cycle.

If the ‘climate sceptics’ could all read from the same hymn book there would be a much better chance of dismissing ‘climate change hysteria’ that is resulting in gross manipulation of energy markets and making it impossible for poor people in cold climates to keep warm in winter while denying many countries who are yet to industrialise the cheap energy that is required to fuel machines. That we have ‘luke warmers’ who consider that man is having some effect on the climate but can’t work out just ‘how much’ influence he is having plays into the hands of the so called ‘consensus’ claimed by the alarmists. This is like reaching down with a machete and cutting your legs off just below the knees. There is no need. Luke warmers…… forget about the theory and OBSERVE.

1910-39 THIRTY YEARS OF COOLING IN THE DAILY MINIMUM AND MAXIMUM

Min 1910-39

Max 1910-39
Fig 2 1910-1930, Daily maximum and Minimum temperatures. Solid line shows trend. Dotted line is a true horizontal.

Above we see that the annual range varies a lot. This is because in the height of summer the ozone content of the air is much affected by what is happening in the Arctic stratosphere. Less ozone means cooler temperature aloft and more cloud. In the depth of winter the ozone content of the air and hence its temperature, cloud cover and the entire global circulation is driven predominantly from Antarctica. If ozone partial pressure falls temperatures at all levels in the atmosphere respond, first in the stratosphere and next in the overlapping region where ozone exists in the upper troposphere and finally at the surface.

Gordon Dobson  put the matter in perspective when he calculated that if the entire atmosphere had the same density that it exhibits at the surface it would have a sharp top at 8 kilometres in elevation. I would remind you that  you can walk 8 km in an hour and if you are a walker in the Olympics you could be there in half an hour.

1940-75 THIRTY YEARS OF COOLING DAILY MINIMUMS AND WARMING DAILY MAXIMUMS

Max 1940-1975

MIn 40-75
Fig. 3 1940-1975  Dotted line is the horizontal

There are two possible reasons why the daily maximum could rise while the daily minimums fall.

  1. Cloud cover could fall away in summer as surface pressure rises in the mid latitudes (along with upper air temperature and geopotential height) while the winds that drive the circumpolar current accelerate due to the enhanced difference in the surface pressure between the mid latitudes and the poles. This would bring colder water from the poles to the western coasts of the southern continents reducing the winter minimum temperature and in fact the summer minimum because when the sun is not shining it matters little whether there is cloud or not.
  2. If the wind blows more consistently from the continent in summer that wind will be hot. That could occur if the core of anticyclones tracked further south. When surface pressure rises in the mid latitudes that is what happens. It has been observed that the so called Hadley cell that takes in the convection in the tropics and the descending air in the mid latitudes  has expanded in recent times. Notice the large fluctuation in the maximum temperature at Cape Leeuwin in summer. Notice that the pattern of extremes is quite different from year to year. This is what determines the level of success I have ias a wine maker in making wine from the early ripening Pinot Noir, a grape that is negatively affected by heat in the last month of ripening. Our ‘Three Hills’ vineyard is just 12 km north of the the lighthouse.On a hot day in February the temperature can climb to 42°C and the relative humidity drops from 60% to 30%. In just one day of this sort of treatment the grapes shrivel and sugar concentration rockets. Fortunately even if February is warm, most of the reds ripen in March and are picked in April. The chance of hot days is less in March, unheard of in April.

Group 1940-75

Above, we give a closer inspection of the temperature profile in the summer of 1958-59. It would not be possible to ripen grapes in such a year. Notice the low variability in the daily data in summer and the relatively high variability in spring. Quite atypical. The diminished area under the summer season temperature curve represents a reduced capacity for plant work.

Global data for the latitude band 30-40° south latitude is not  necessarily representative  of local conditions at Cape Leeuwin but neither of the summers of 1956-7 or 59-60 look particularly auspicious when we  examine the  geopotential height data for these years. Heights are likely to vary less with latitude than is sea surface temperature.  Sea surface temperature depends on the circulation of the ocean that exhibits a south to north and north to south component  whereas the movement of the atmosphere has a gently north east to south east movement that comes pretty close to following lines of latitude.

SST and GPH

1975-1992 COOLING DAILY MAXIMUMS AND COOLING DAILY MINIMUMS

Max 1975-92

Min 75-92

In this graph we have fewer years and the pattern of heightened variability in mid-summer and mid-winter is  more apparent to the eye. Year to year variability comes from the same source as long term variability, the winter pole with peak variability in January-February emanating from the Arctic and July-August from the Antarctic. This is what is behind the variation in the seasons that keeps the farmers guessing.Its also what lies behind the long term variability, decadal and longer.

1992-2015 A STRONG WARMING CYCLE FOR THE MAXIMUM AND LESS SO FOR THE MINIMUM….OR IS IT?

 

Max 92-15

 

Min 75-92

Again the dotted line is the horizontal. Its easy to see that the minimum has increased at about half the rate of the maximum. There is nothing in the Earth system that takes away carbon dioxide overnight and puts it back in the daytime.

sculpt

Magnification drives home the point that variability in temperature is strongest in mid winter and mid summer. Extreme summer variability is due the fact that Cape Leeuwin occasionally experiences hot winds from the East in summer but it is also due to a flux in the ozone content of the air above and with it, cloud cover. Autumn is a time of low variability, balmy pleasant weather with light winds. The coldest months of winter are not always cold and nothing in the shape of the curves  in the bridging seasons provides any sort of an indication of what will happen in June, July, August and September. That depends on whats happening at the Antarctic circumpolar front.

Max 92-15.JPG  second

min 92-15.JPG second

Above is a different way of looking at the same data for the last 23 years. The trend curves are polynomials and they fit better the pattern exhibited by the extremes. The cooling trend of the last five years is given the weight it deserves. So far as the minimum is concerned we will soon be back at where we started in 1910.

THE VIRTUE OF DIS-AGGREGATION OF TEMPERATURE DATA

In the figure below we have data for the entire globe in the 30-40° south latitude band drawn from here.

30-40S glabally Feb and July
Fig 5.  Sea Surface Temperature 30-40° south. Average monthly data.

Average monthly data conceals the interesting complexities that are only revealed in daily maximums and minimums. Is the temperature increasing during the day or at night? We are at a loss to explain anything and we are at the mercy of witch doctors who rush in to provide us with a global average.

At Cape Leeuwin the  daily maximum is the chief driver of variations in the average temperature.  Without a shadow of a doubt part of that daytime summer warming is associated with loss of cloud as the increase in geopotential height and air temperature aloft suggests. Part will be due to a more easterly component in the air in the summer that brings warm air from the warming continent during the day. In any case, its readily apparent that the direction of the wind can be critical to surface temperature in coastal locations. That applies, not only in coastal locations, but everywhere, when the wind comes more consistently from either the equator or the pole. Change the wind and you change the local temperature. For this reason we need to get a grip on what changes the global circulation if we wish to understand surface temperature change. Just quietly, we also need to get a grip on the degree of mixing of cold deep water with warm surface water due to the currents and the waves. We are measuring the temperature of our patient not in his anus or his mouth or ear-hole but at the extremities.

Some of the change in temperature at Cape Leeuwin may well be due to a change in the amount of cold water from the Southern Ocean being driven up the coast due to an increase in the speed of the southern ocean circulation. In that case, the enhanced current will tend to limit the increase in the temperature of the air as measured at Cape Leeuwin. The enhanced pressure differential between the mid and high latitudes has undoubtedly enhanced the circumpolar circulation and assisted to stabilise the temperature at Cape Leeuwin, a built in countervailing force limiting the rate of temperature increase due to loss of cloud cover and a generally enhanced flow of warm air from the tropics as the Antarctic circumpolar trough in surface pressure has deepened.

 

34 LOCAL WEATHER

My impression is that  winter of 2016 has been unusually cold. But rather than trust my senses I went looking for data.

Cape Leeuwin is the closest station in the Australian ACORN network. The stated purpose of the network is to maximise the length of record and the breadth  of the coverage across the country.

The Cape Leeuwin lighthouse sits on a granite rock where the Southern Ocean meets the Indian Ocean at 34° 34′ south latitude. When the wind blows from the west it is the Indian Ocean temperature that is being sampled and when it blows from the north east its the air coming off the Australian continent. Three lighthouse keepers cottages made of local limestone sit in the lee of the lighthouse and the wind blows day and night.  At the rear of each house stands an external wash house with an old fashioned twin basin concrete trough and a wood fire heated ‘copper’ for boiling water. Its a lonely spot but the fishing is good. The nearest centre of population to the west is Cape Town.

Leeuwin position
Fig 1 South West of Western Australia, weather data stations on the Acorn network.
Cape Leeuwin
Fig. 2 Temperature at Cape Leeuwin lighthouse.

Black lines record the linear trend as calculated by Excel and indicate cooling. Red dotted lines track the highest summer maximums and the lowest winter minimums and they have a very similar slope to the black trend lines. Horizontal lines enable us to see that the minimum has declined by 0.7°C and the maximum by about 1°C. We know that over the last  five years there has been warming in the tropics that compares in its intensity to that seen prior to 1998. The trend at Cape Leeuwin is directly opposed to that.

ENSO 3.4

Notice the deformation of the curves in mid summer and the skinny little peak in 2014-15, not a good year to be trying to ripen a crop of grapes.

When the air blows off the continent in a warm year the temperature can reach 40°C but that is rare. By contrast there is very little variation in the minimum temperature but it does vary more in winter than summer.

The deformation of the winter minimums looks like ‘shark attack’. This is driven from the Antarctic. It works this way: A change in the intensity of polar cyclone activity in high latitudes modifies the differential pressure between the mid latitudes and the poles and also cloud cover. But for this influence we would see something like a smooth sine wave at the turning points in summer and winter. The beauty of having data for the minimum and the maximum temperatures is that you see the patterns of variability. When you average you lose information. The bits you lose are vital.When you average the temperature for the whole globe you are either a fool or a knave and I would immediately expect that you have an agenda to push.

I will describe the warming cycle that applies to the mid latitudes in the southern hemisphere but before I do let me suggest that these latitudes are very important to the global heat budget because water absorbs energy and acts like a battery and these latitudes are almost an uninterrupted sweep of water: When surface pressure falls at the pole it is accompanied by a warming of the stratosphere due to a build up in ozone. The falling pressure at the pole induces an enhanced flow of warm air from the equator.  Cape Leeuwin then warms in the middle of winter because the air comes from a warm place. At the same time more ozone descends in the mid latitude high pressure cells. Ozone warms by absorbing infrared. The warming of the air reduces cloud cover allowing extra solar radiation to reach the surface. In meteorological terms there is an increase in geopotential height as the atmospheric column warms, a reduction in cloud cover, that you could never directly measure, but you can infer the fact due to the fact that the surface warms. The cooling cycle is the reverse. It starts with a reduction in the ozone content of the air in high latitudes and rising surface pressure in the mid latitudes as polar cyclone activity falls away. Increased cloud cover cools the mid latitudes and cold air from the south finds its way more frequently into the mid altitudes.

The last seventy years has brought a secular decline in surface pressure in high latitudes and an increase in surface pressure in the mid and low latitudes as is apparent in figure 3. Nowhere is surface pressure higher than in the 30-40°  south latitude. The latitude of Cape Leeuwin  is 34° 34′ south. This latitude is home territory for a travelling band of enormous high  pressure cells of relatively cloud free air. When pressure increases cloud cover falls away.

pressure
Fig. 3 Evolution of sea level atmospheric pressure in the southern hemisphere since 1948.

The seventy year increase in surface pressure and the parallel increase in sea surface temperature in the low and mid latitudes of the southern hemisphere is documented in figure 4

SST and Surface pressure 1
Fig. 4

Figure 5 reveals that surface pressure at 40-50° south has risen very little while surface pressure at 50-60° and 60-70° south latitude has declined strongly. That is a function of relative area. Not shown is surface pressure over the polar cap that closely follows the trends at 60-70° south.

SST and SLP
Fig. 5

Notice that sea surface temperature rises and falls with  surface pressure throughout. This relationship is good for change in both directions in both the short and the long term. Notice the marked discontinuity in surface temperature at 60-70° south after 1976.

Naturally, the temperature increase across the latitude bands is uneven. The largest whole of period variation of 2°C is seen at 60-70° of latitude due to the increased incidence of warm north westerly winds with an abrupt shift between 1976 and 1978. The more or less parallel behaviour in the curves since that time is what we observe in mid and high altitudes, a classic cloud cover/wind direction response that occurs on short term like daily and monthly time scales, and also long term, annual, decadal and longer time scales. This response to the ozone content of the atmosphere drives short term change like that observed in figure 2 and long term change that I will document in the next post that will be devoted to one hundred and six years of data from Cape Leeuwin a treasure trove of  temperature information due to the diligence of lighthouse keepers in patiently recording the minimum and the maximum temperature every day, except on those few days where, unaccountably, they didn’t.

The next largest variation in temperature  is seen in the tropics where variation in the intake of cold waters from high altitudes gives rise to big variations in sea surface temperature that are unrelated to cloud (very little anytime) or winds (very light). The next largest variation is in the latitude of Cape Leeuwin at 30-40° south where the  variation is 0.97°C. This core region for travelling anticyclones of descending air. These HIGHS are greatly susceptible to variations in geopotential height that proceed in concert with surface temperature. This is documented in figures 6 and 7.  Increased geopotential height always brings warming.  The contrast in temperature according to wind direction is less here than in high latitudes adjacent to the Antarctic ice cap. It is safe to conclude that the response of surface temperature to increased geopotential height in low and mid latitudes is chiefly due to a change in cloud cover.

SST and GPH low
Fig 6
SST and GPH high
Fig 7

In examining this data one must remember that geopotential height is simply the height of a pressure surface. For example the 500 hPa  pressure level is found on the average at 5500 metres above sea level. When the air below that pressure level is warmer, geopotential heights will exceed 5500 metres and the warmer the atmospheric column the higher one has to go to get to the pressure surface. Heights change on daily and weekly time scales and are clearly associated with change in surface temperature and cloud cover. High heights are associated with high pressure anticyclones that bring fine sunny weather. At Cape Leeuwin low heights are associated with polar cyclones, high winds, cloud streaming in from the north west and frontal rainfall. The latter is the winter pattern and the former is the summer pattern.

There is also a close relationship between air temperature and the geopotential height at particular pressure levels as we see in Fig 9 and 10. In these figures we are looking at  heights at the 200 hPa level where the presence of ozone is associated with Jet stream activity. When heights vary at 200 hPa they  vary in the same direction at 500 hPa and 700 hPa because in these high pressure cells the air constantly descends. Cloud can be found at all levels, especially in the early part of the day. Clouds that exist as multi branching crystals of ice  have a relatively large surface area are highly reflective.

Temp and GPH low
Fig 9
Temp and GPH 2
Fig 10

Notice the overt expression of the 1976 climate shift between 15° south and 40° south where anticyclones circulate. This change is expressed as the jump in sea surface temperatures in the tropics as seen across the latitude bands in figure 6 and even more so at 60-70° of latitude in figure 7 where change in the wind direction is associated with a large change in surface temperature.

Notice also the strong drop in surface pressure at 50-60° south in the 1990’s that is associated with a fall in geopotential heights and also sea surface temperature.

What is described here is not new to ‘climate science’ as it existed fifty years ago. But most of the cohort of scientists that learned their trade in the satellite age will be unfamiliar with this train of thought.

Edward N Lorenz of the Massachusetts Institute of Technology back in 1950 published an article entitled  ‘The Northern Hemisphere Sea-level Pressure Profile’ and the abstract reads as follows:

The variations of five-day mean sea-level pressure, averaged about selected latitude circles in the northern hemisphere, and the variations of differences between five-day mean pressures at selected pairs of latitudes are examined statistically. The northern hemisphere is found to contain two homogeneous zones, one in the polar regions and one in the subtropics, such that pressures in one zone tend to be correlated positively with other pressures in the same zone and negatively with pressures in the other zone. Considerable difference is found between the seasonal and the irregular pressure-variations which result from mass transport across the equator, but the seasonal and the irregular variations of pressure differences resemble each other closely, as do the seasonal and the irregular pressure-variations which result from rearrangements of mass within the northern hemisphere. The most important rearrangements appear to consist of shifts of mass from one homogeneous zone to the other. These shifts seem to be essentially the same as fluctuations between high-index and low-index patterns. The study thus supports previous conclusions that such fluctuations form the principal variations of the general circulation, and also shows that, except at low latitudes, the seasonal pressure-variations are essentially fluctuations of this sort. The possibility that the seasonal and the irregular variations have similar ultimate or immediate causes is considered. 

Prior to 1979 when satellites were used to obtain data for the entire globe very little was known about the Southern Hemisphere where the most powerful driver of the atmospheric circulation is to be found. Although the Arctic Oscillation had been well documented the Antarctic Oscillation had not. Lorenz did not have the data at his disposal. Today we do. But, nobody is looking!

At one time people were aware that the surface pressure relationship between the mid and the high latitudes changed over time. Nobody knew why. Some canny researchers documented a correlation with geomagnetic activity implicating  the solar wind but the  actual mechanism  eluded them.

Gordon Dobson’s students explored this issue as soon as they had a single years data for total column ozone as he recalled in 1968 in his lecture ‘Forty Years Research on Atmospheric Ozone at Oxford: a History’, in these words:

Chree, using the first year’s results at Oxford had shown that there appeared to be a connection between magnetic activity and the amount of ozone, the amount of ozone being greater on magnetically disturbed days. Lawrence used the Oxford ozone values for 1926 and 1927 and in each year found the same relation as Chree had done. 

Early observers of ‘sudden stratospheric warmings’ had a suspicion that the phenomena were somehow connected with the sun. Researchers like Van Loon and Labiske pointed out that the solar cycle was clearly associated with aspects of the behaviour of the stratosphere.

But these lines of investigation became matters for the fringe dwellers in the atmsopheric sciences, the sort of people who don’t get invited to dinner parties, when Houghton took over from Dobson at Oxford , a mathematician and a physicist and a devotee of the notion that the carbon dioxide content of the atmosphere governed near surface temperature. At that point climate science fell into a hole of superstition and conviction based not on observation but ‘belief’. Climate science morphed into a religion. Houghton went on to chair the IPCCC body responsible for linking the activities of man with climbing surface temperature. Naturally at that point climate science then began to attract a lot of interest and funding, particularly in the United States where NASA under James Hansen saw the opportunity to create a role for itself in keeping an eye on what was happening. The time of the self funded gentleman scholar, like Dobson was over the time for proselytisers had arrived and the gravy train was immense. Even Australia’s CSIRO had a cohort of more than a hundred scientists working on the problem.

To this day there is no appreciation of the origin of the circumpolar trough of very low surface pressure that surrounds Antarctica.  There is no appreciation of the role of ozone in creating that trough or its role in driving high wind speeds in that part of the upper troposphere that overlaps with the lower stratosphere, the origin of upper air troughs, no appreciation of how these troughs propagate to to surface to initiate a ‘cold core’ polar cyclone. Where ignorance and superstition rule the day there can be no appreciation of the role of the polar atmosphere in driving the entire circulation, the atmosphere super-rotating about the planet in the same direction as the planet spins but faster at higher latitudes and altitudes, fastest at the point where the atmosphere begins to conduct electricity (although it does so all the way to the surface) where it dances to the tune of the solar wind. The notion that the Earth exists in an interplanetary environment held in ordered embrace by  electromagnetic fields where the atmosphere is the outer mobile skin that is first  affected by those forces and so driven to rotate and thereby to some extent dragging the Earth with it, the whole apparatus working like clockwork that is forever wound up by the thermonuclear furnace at its very core….all thoughts of this nature are now anathema.

One could give most of the climate scientists trained since the start of the satellite age free membership of the Flat Earth Society. They would fit in very nicely.

IF CAPE LEEUWIN HAS BEEN COOLING WHILE AN EL NINO EVENT HAS BEEN BUILDING IN THE TROPICS WHAT HAS  BEEN HAPPENING ON THE EAST COAST OF AUSTRALIA?

Coffs long
Fig 11 Coffs Harbour 20 years minimum daily temperature

Coffs Harbour is 3° of latitude closer to the equator than Cape Leeuwin. This coastal town is subtropical and is the home of the Big Banana. It experiences a 12°C range in its minimum  as against 8°C at Cape Leeuwin. Cold air flows off the continent in winter driving the minimum lower. The other main driver of local temperature is the temperature of the  ocean waters flowing southwards down the coast. Warm water is present in winter in El Nino years due to the build up of warmth across the tropics and the anticlockwise rotation of the Pacific Ocean. It is in winter that the differential pressure driving the westerlies of the southern hemisphere is  at its maximum speeding the flow of the Antarctic circumpolar current that flows northwards towards the equator on the eastern sides of the Ocean basins and southwards on the western sides of the ocean basin. In this circumstance one would expect change in the winter minimum at Coffs simply because the winds that drive the currents blow harder in winter. I refer of course to the roaring forties the furious fifties and the screaming sixties.

The dotted lines at  the limits of the range are horizontal. Judged by eye, they indicate no warming or cooling.  The trend calculated by XL descends.

Nowhere in the course of this analysis have I referred to carbon dioxide in the air, a matter  that is irrelevant to atmospheric dynamics and the course of change in surface temperature. In the next chapter I look at 106 years of data from Cape Leeuwin that is as representative of conditions in the Southern Indian Ocean, as you are likely to find in the data from a single weather station..

 

33 SURFACE PRESSURE AND SUNSPOT CYCLES

SLP Jan
Fig. 1 Sea surface atmospheric pressure in January Source here

Even in the height of summer we see a marked trough in surface pressure on the margins of Antarctica, a product of polar cyclone activity driven by differences in the ozone content of the air and resulting differences in air density. Of course, the contrast  between the coldness of the ice bound continent and air from the mid latitudes also helps but at 200 hPa where these cyclones are generated the contrasts seen at the surface are less apparent. Surface contrasts probably assist in allowing the upper air troughs to propagate to the surface but where these contrasts don’t exist as in Arctic summer the propagation from upper air troughs to the surface to create a polar cyclone still occurs.

January pressure
Fig 2

In winter atmospheric pressure increases in the mid latitudes of the southern hemisphere increasing the differential pressure between the mid latitudes and 60-70° south. Surface pressure over Antarctica hits a planetary maximum.

July pressure
Fig. 3  Source of data for FIgs 2 and 3  here:

Figures 2 and 3 show the swings in pressure that are part of the annual cycle and the evolution of pressure over time. Mainstream climate science (is there any other) has yet to realise the importance, let alone account for the cause of that massive deficit in surface pressure in the ocean about the margins of Antarctica. ‘Climate science’ is yet to become aware  of the cumulative effect of the decadal slips in surface pressure and is incapable of making the connection with the ‘annular modes phenomenon’ or working out that the atmosphere is driven from the poles rather than the equator, let alone working out the mechanisms involved.in change. Perhaps this is because the bulk of the land mass and the population of the globe together with most of the money is in the northern hemisphere and perhaps because the Earth is round the incumbents can not see over the equatorial horizon?

WHATS HAPPENING WITH SURFACE PRESSURE IN ANTARCTICA?

SLP 80-90S by month
Fig. 4 Source of data here.

In FIG 4 the year to year variability is perhaps due to change in the rate of intake of mesospheric air into the stratosphere as it modulates the partial pressure of ozone above the 300 hPa pressure level.  The change in surface pressure  is greatest in Antarctica but it  impacts the global atmosphere from pole to pole. The southern hemisphere vortex is most influential in determining the ozone content of the air between June and November and the northern vortex between November and April.

AO and AAO
Fig 5 Source of data here.

The Arctic Oscillation and the Antarctic Oscillation indices are proxies for surface pressure over the pole. As they fall, we know that surface pressure rises over the pole. We see in fig. 5 above that a rise in the AAO, signalling a fall in surface pressure in the Antarctic forces an increase in surface pressure in the Arctic between June and November whereas the weaker, poorly structured and migratory northern vortex seems to be incapable of the same performance when it is active in northern winter. Perhaps our measurement  settings are not capturing it adequately.

The replacement of low ozone content air with high ozone content air consequent on a stalling of the intake of mesospheric air brings an increase in the temperature of the stratosphere. The greater the elevation the greater is the increase in temperature, a natural product of the fact that ozone is the agent of convection and it is ozone rich air that is lifted to the limits of the atmosphere.   This amplified response is documented at 80-90° south latitude in figure 6 below.

T of Sth Strat at 80-90S Lat
Fig 6 Source of data here.

Plainly, the largest response to an increasing presence of ozone is at the highest elevations. There has been a fundamental change in the temperature profile over the polar cap with a massive shift  from 1976 to 1978. Note that prior to this date the temperature at 10 hPa was little different to that at 200 hPa. The 200 hPa level is Jet stream altitude.What happens at 200 hPa determines the synoptic situation and is reflected at lower altitudes albeit, softened and smoothed due to the fact that not all activity at 250 hPa propagates all the way to the surface. Upper level troughs are cyclones that are insufficiently strong to  propagate all the way to the surface.But the point to be aware of is that the temperature profile between 200 hPa and 10 hPa is fundamental to the dynamics determining the movement of the atmosphere over the pole that relates to the timing of the final warming.

VARIABILITY AT DIFFERENT TIMES OF THE YEAR

Another way to assess the impact on the Antarctic stratosphere is via a whole of period assessment of temperature variability at 10 hPa according to the month of the year. To examine this each months temperature is ordered from highest to lowest regardless of the year attached to the data and the difference between the highest and lowest is derived. That difference is graphed In Fig. 7

Variability in 10hPa temp by latitude
Fig 7 Source of data here.

It is plain from  Fig 7 that in the period between 1948 and 2015 temperature variability in high southern latitudes is greatest between July and October. At lower latitudes variability is strongest in June or at the start of the year. The skew towards October reflects the impact of a developing ozone hole below 50 hPa that is forced by the intake of troposphere air containing the ozone destroyer, NOx that is drawn in laterally between 100 hPa  and 50 hPa like a gradually tightening hangman’s noose that by September occupies the entire polar cap. Very cold air drawn in from the equatorial upper stratosphere is as cold as air from the mesosphere but it has more NOx, a catalyst for the destruction of ozone. This produces a severe contrast in ozone partial pressure and air density across the vortex, generates intense polar cyclone activity and drives surface pressure at 60-70° south to its annual minimum when the hole is fully established.

the ozone hole
Fig 8 Source of data here

Fig. 8 shows NOx at 50 hPa . By 15th October 2015 NOx has destroyed all ozone between 100 hPa and 50 hPa as we see at left in Fig 9 below in terms of the distribution of ozone. The light blue line defines the position of the vortex at 50 hPa.

12th Oct
Fig 9 Source of data at left and right 

In  Fig 9,  above at right, the dotted black line represents  ozone prior to the establishment of the hole while the purple line shows the temperature profile at that time. The red line shows that temperature increases as the hole establishes in stark contrast with the narrative of those who promote the story that man is responsible for the hole, a natural feature of the polar atmosphere in spring. Big Green prefers ‘unnatural’ and it would muddy the narrative if they had to admit that the hole is a natural consequence of atmospheric dynamics.

The contrast between cold air devoid of ozone and warm air from the mid latitudes that is rich in ozone at 60° south seen in figure 9 at left drives intense polar cyclone activity giving rise to a springtime minimum in surface atmospheric pressure as seen in figure 10. It was there in 1948 but more so in November. As surface pressure has fallen and ozone partial pressure has increased the minimum is a month earlier.

SLP 60-70°S
Fig. 10 Source of data here.

The winter maximum in surface pressure seen in Fig 10 now occurs earlier than it did in 1948.

Below we see that the climate shift of 1976-8 shows up in the comparison between sea surface temperature and the temperature of the air 200 hPa (where ozone warms the air) at 25-35° south latitude. This represents enhanced ozone propagating across the latitude bands at the time of the 1976-8 climate shift, a shift that simultaneously intensified the Aleutian low in the North Pacific, the dominant low pressure, ozone rich area in the northern hemisphere with knock on effects across the Pacific and North America.

25-35°S
Fig 10 Source of data here

The increase in the temperature at 200 hPa produces an increase in geopotential height. There is a well established relationship between GPH and surface temperature as acknowledged and demonstrated in the paragraph below from the US National Oceanic and Atmospheric Administration under the heading ‘Temperatures’. What a title!

NOAA statement

In this way the ozone content of the atmosphere is linked to the synoptic situation, the generation of the jet stream, upper level troughs and polar cyclones. Polar cyclones are the most vigorous and influential elements in the circulation of the atmosphere and the prime determinant of the rate of energy transfer from torrid equatorial to frigid high latitudes because they determine the pressure gradient between the equator and the pole. The warm moist westerly winds emanating from tropical rain forests pass by the high pressure systems of the mid altitudes and drive pole-wards warming the surface and giving rise to precipitation in ‘fronts’.

If the jet stream loops towards the equator cold dry polar winds sweeps equator-wards bringing near freezing conditions to mid and even low latitudes. Orange Orchards in subtropical Florida can be frosted. Cold Antarctic Air has been known to sweep northwards into Brazil. If polar atmospheric pressure increases the mid latitudes cool due to this influence and also due to increased cloud cover under high pressure systems as geopotential heights fall away with the ozone content of the air.

The progressive loss of atmospheric mass in high southern latitudes over the last seventy years has added mass to the mid altitudes and enhanced the westerly wind flow while opening up the sky to admit more solar radiation thereby warming the oceans. The result has been a marked warming of the air in high southern latitudes centred on those months where this natural variability occurs, primarily between Jun and the ozone hole months of the Antarctic springtime. See Fig 11 below.

A peculiarity  in the Antarctic record is the cooling experienced in summer over the last seventy years. The Arctic forces atmospheric mass into  high southern latitudes as it becomes ozone-active in the months November through to February keeping the westerlies at bay in the summer season giving rise to cooling in high southern latitudes.

60-90S
Fig 11 Source of data here

THE EVOLUTION OF SURFACE PRESSURE OVER THE LAST SEVENTY YEARS AND ITS POSSIBLE RELATIONSHIP WITH THE SUNSPOT CYCLE

SLP Antarctica
Fi 12 source of pressure data here

Sunspot numbers: Source: WDC-SILSO, Royal Observatory of Belgium, Brussels

 

The decline of surface pressure at 80-90° south latitude is punctuated with oscillations between regimes of relatively high surface pressure that are on average about 3.5 years apart with twenty such occurrences in the last sixty nine years and an equivalent number of periods of low surface pressure. The amplitude of the swings varies little within a solar cycle but secular change seems to occur between solar cycles. Change points seem to be associated with solar minimum.

If we now superimpose the data for surface pressure  in the high Arctic we have Fig. 13:

Polar SLP
Fig 13

Remarks:

  • Over time we see a shift of atmospheric mass from the poles and a gain of mass in the region of the East Asian High pressure zone. In fact atmospheric mass is likely to accrue everywhere except in high latitudes above 50° where polar cyclones, energised by increase in the partial pressure of ozone force pressure reductions. This process has fundamentally changed the parameters of the climate system. Changed, not ‘warped’ because warping suggests something unnatural and change is a natural and ongoing process. The change in 1976-8 involved a marked drop in Antarctic surface pressure that forced an increase in Arctic surface pressure regardless of the increase in global ozone at that time. The change in surface pressure has been continuous and  frequently abrupt and in particular either side of the relatively spotless cycle 20. There is a change of slope between 21 and 22 that is common to both hemispheres.
  • The evolution of surface pressure is characteristically different in different solar cycles
  • In solar cycle 18 Antarctic atmospheric pressure is superior to that in the Arctic. This superiority disappears in solar cycle 19, the strongest of recent times.
  • The very strong solar cycle 19 saw a steep fall in atmospheric pressure over Antarctica and also over East Asia but a compensating increase in pressure in the Arctic.
  •  The weak solar cycle 20 that nevertheless exhibited strong solar wind activity, saw a fall in atmospheric pressure at the poles that proceeded ‘hand in hand’  and a strong compensatory increase in surface pressure over the Eurasian continent.
  • The climate shift of 1976-8 involved a departure from the norm of the previous solar cycle 19 in that extreme falls in atmospheric pressure over Antarctica produced short term mirror image increases in Arctic surface pressure. Antarctic pressure still declined at much the same rate as it had over cycle 20 prior to the climate shift of 1976-8 .
  • Cycle 22 sees a recovery in Antarctic pressure and a compensatory collapse in Arctic pressure now establishing at the lowest level seen in the entire 69 year period bringing on the period of strong  advance  in Arctic temperature and loss of sea ice.
  • The onset of further declines in Antarctic pressure in cycle 23 allowed a recovery in Arctic pressure that, despite stepping to a higher level at the start of the cycle, declined over the period. Mirror image effects are again apparent.
  • Cycle 24 brings a brief recovery in Antarctic pressure at the expense of the Arctic where the peaks decline quickly as successive minimums in Antarctic  pressure (except the last) are higher than the previous minimum.
  •  After solar maximum in cycle 24 the decline in surface pressure in Antarctica is spectacular involving  greatly enhanced polar cyclone activity  perhaps due to enhanced ozone production due to  increased  cosmic ray activity as solar cycle 24  enters the decline phase. Reduced sunspot and flare activity  is responsible for a very compact atmosphere that may react more vigorously to the solar wind.
  • The peak in Eurasian surface pressure occurred about 1998 and a slow decline appears to have set in.

Generalising we can say that surface pressure and surface temperature appears to be linked to solar activity but in a fashion that is completely different to the narrative that insists that ‘total solar irradiance’ is the the only factor of importance. Rather, the driver of natural change in climate  works by changing the planetary winds and cloud cover via polar atmospheric dynamics that are closely linked to the flux in the ozone content of the air. Since 1978 the swings in surface pressure in Antarctica have been vigorous suggesting that a more compact atmosphere reacts more strongly to change in the solar wind and that cosmic rays that are enhanced in a regime of low solar activity may be more influential in ionising the polar atmosphere allowing the generation of ozone and especially so  during periods where the intake of mesospheric air is disrupted and the polar stratosphere warms. It is apparent that the ozone content of the air in high latitudes peaks in late winter/spring  even though the lifetime of ozone in the atmosphere is progressively shortened due to the increase in the incidence of destructive UVB radiation as the sun rises higher in the sky and the earths orbit takes it closer to the sun. Something has to account for that extra ozone. Climate science does not even pose the question, let alone answer it.

The ‘canary in the coalmine’ that indicates the change in the forces at work can be seen in extreme surface temperature variability in February and July. These months exhibit the greatest differences in terms of the whole of period  minimum and whole of period maximum in surface pressure as seen below. It is the months of January and July that exhibit the greatest variability in surface temperature. We see that in the sphere of natural climate change, surface pressure and surface temperature are inextricably linked. But, then again we always knew that by looking at the weather from week to week.

SLP varn Antarctica
Fig 14

The evolution of Antarctic surface pressure by the month is explored in the third diagram in this chapter. It appears that the system is at a turning point. Eight of the twelve months of the year, including the critical months under the control of the Antarctic and later the Arctic, from August through to February  show signs of a rise in surface atmospheric pressure. If this continues and the  ozone content of the global atmosphere continues to fall, and with it the temperature of the upper stratosphere we might sometime witness a reversal of the climate shift of 1976-8.

TEST QUESTIONS related to Fig.15: Have you understood this chapter?

Why is it that the Antarctic stratosphere above 150 hPa warms faster than the  atmosphere below 150 hPa in spring?

Why do we see the abrupt change in slope in the temperature of the air above 70 hPa in November?

Why does temperature between the surface  and 400 hPa decline at an invariable rate between April and August while the atmosphere above becomes increasingly colder?

What is the temperature at the tropopause in August and at what elevation is it located?

Query
Fig. 15

 

POSTSCRIPT:   For the convenience of the reader I list the chapters in this treatise in order to provide an idea of the scope of the work and the manner of its development. At the end is a list of chapters currently in preparation.

Reality

How the Earth warms and cools in the short term….200 years or so…the De Vries cycle

Links to chapters 1-38

  1. HOW DO WE KNOW THINGS Surface temperature is intimately tied to the global circulation of the air and the distribution of cloud.Ozone is inextricably linked to surface pressure and cloud. The key to unlocking the cause of climate change lies in observation.
  2. ASSESSING CLIMATE CHANGE IN YOUR OWN HABITAT On accessing and manipulating data to trace the way climate changes regionally. It is essential to understand the manner in which the globe warms and cools if one is to correctly diagnose the cause.
  3. HOW THE EARTH WARMS AND COOLS NATURALLY It is observed that the surface warms when geopotential height increases. This chapter answers the question why geopotential height increases.
  4. THE GEOGRAPHY OF THE STRATOSPHERE  Answers the question ‘at what elevation does the incidence of ozone cut in as a means for heating the atmosphere thereby creating what has been erroneously described the ‘stratosphere’. In winter its anything but stratified. It should be renamed ‘The Startosphere’.
  5. THE ENIGMA OF THE COLD CORE POLAR CYCLONE High latitude cyclones are the most vigorous circulations on the planet. At the surface they have a cold core. Their warm core is in the upper troposphere where the ozone impinges. No cyclone can form without a warm core.
  6. THE POVERTY OF CLIMATOLOGY Geopotential height at 200 and 500 hPa vary together in the extra-tropical latitudes. Furthermore, the increase in geopotential height that accompanies the surface pressure change is accompanied by a loss of cloud cover. All ultimately relate to the changing flux of ozone in the upper half of the atmospheric column in high latitudes.
  7. SURFACE TEMPERATURE EVOLVES DIFFERENTLY ACCORDING TO LATITUDE Surface temperature change is a two way process that occurs at particular times of the year.
  8. VOLATILITY IN TEMPERATURE. Temperature change is a winter phenomenon, increasing in amplitude towards the poles
  9. MANKIND IN A CLOUD OF CONFUSION Our understanding of the atmosphere is primitive.
  10. MANKIND ENCOUNTERS THE STRATOSPHERE. The origin of the stratosphere was a mystery back in 1890 and we still haven’t got it right.
  11. POPULATION, SCARCITY AND THE ORGANISATION OF SOCIETY. A dispassionate view of the Earth, considering its ability to promote plant life, sees the planet as distinctly cooler than is desirable.
  12. VARIATION IN ENERGY INPUT DUE TO CLOUD COVER. The atmosphere mediates the flow of solar energy to the surface of the planet via change in cloud cover. How could this be overlooked?
  13. THE PROCESSES BEHIND FLUX IN CLOUD COVER. A discussion of some of the intricacies involved in the relationship between surface pressure, cloud cover and the uptake of energy by the Earth system.
  14. ORGANIC CLIMATE CHANGE A discussion of the big picture that focuses on the natural sources of climate change.
  15. SCIENCE VERSUS PROPAGANDA The scare campaign about ‘global warming’ or ‘climate change’ is not based on science. Science demands observation and logic.  There is a ‘disconnect’ between observed change and the hypothesis put forward to explain it. One cannot ‘do science’ in the absence of accurate observation. What is being promoted as ‘Climate Science’ by the UNIPCC fails at the most basic level.
  16. ON BEING RELEVANT AND LOGICAL Climate scientists freely admit they do not know what lies behind surface temperature change that is natural in origin that expresses itself regionally and with large differences according to latitude i.e. the annular modes (Arctic and Antarctic Oscillations). In that circumstance it is nonsense to attribute change to the influence of man. There is an error in logic. But, its wilful.
  17. WHY IS THE STRATOSPHERE WARM Is the warmth of the stratosphere due to the interception of ultraviolet radiation or heating due to the interception of long wave radiation from the Earth? This issue is fundamental. Observation provides the answer.
  18. THE OZONE PULSE, SURFACE PRESSURE AND WIND The direction and intensity of the wind and the distribution of ozone is closely related. This chapter gives an introduction to the nature and origin of the annular modes phenomenon.
  19. SHIFT IN ATMOSPHERIC MASS AS A RESULT OF POLAR CYCLONE ACTIVITY The distribution of ozone maps surface pressure. When the partial pressure of ozone builds pressure falls locally and is enhanced elsewhere.
  20. THE DISTRIBUTION OF ATMOSPHERIC MASS CHANGES IN A SYSTEMATIC FASHION OVER TIME Surface pressure changes on long time schedules. UNIPCC climate science is oblivious to these changes and the consequences attached to the change.
  21. THE WEATHER SPHERE-POWERING THE WINDS. The strongest winds can be found at the overlapping interface of the troposphere and the stratosphere and we haven’t yet worked out why or what it means when change occurs at that interface.
  22. ANTARCTICA: THE CIRCULATION OF THE AIR IN AUGUST An introduction to the structure and dynamics of the atmosphere in high latitudes
  23. THE DEARLY BELOVED ANTARCTIC OZONE HOLE, A FUNCTION OF ATMOSPHERIC DYNAMICS. The celebrated ‘hole’ is actually a natural feature of the Antarctic atmosphere in spring and has always been so. It’s dictated by geography and process during the final warming.
  24. SPRINGTIME IN THE STRATOSPHERE More detail on the natural processes responsible for the ozone hole.
  25. WHERE IS OZONE? PART 1 IONISATION. The structure of the upper atmosphere is dictated by process. Hand waving is no substitute for observation.
  26. WHERE IS OZONE PART 2 EROSION More on the processes responsible for the structure of the atmosphere in high latitudes and in particular the manner in which tongues of air of tropical origin are drawn into the polar circulation.
  27. COSMIC RAYS, OZONE AND THE GEOPOTENTIAL HEIGHT RESPONSE Observation and logic suggest that both the solar wind and cosmic rays are independently influential in determining the partial pressure of ozone in high latitudes. No other possibility is remotely plausible.
  28. MISREPRESENTING THE TRUTH Ozone, not UV radiation warms the upper air in winter
  29. THE PURPOSE OF SCIENTISTS History is re-interpreted continuously to suit the purposes of elites. Science is moulded in that same way by virtue of the fact that the elites hold the purse strings. All is ‘spin’.
  30. THE CLIMATE SHIFT OF 1976-1980. The nitty gritty of how climate changes together with the basics of a theory that can explain the natural modes of variation. Observation and theory brought together in a manner that stands the test of common sense.
  31. DIFFERENCES BETWEEN THE HEMISPHERES: THE ORIGIN OF STRATOSPHERIC WARMINGS. Unfortunately climate science has a lot to learn. It has to begin with observation rather than mathematical abstractions. In fact, it’s best to keep the mathematicians at arms length.
  32. THE CLIMATE ENGINE THAT IS THE OZONOSPHERE . The atmosphere re-defined to take account of the critical processes that determine its movements and thereby the equator to pole temperature gradient. Takes a close look at processes inside and outside the winter time polar vortex. The system is the product of the distribution of ozone.
  33. SURFACE PRESSURE AND SUNSPOT CYCLES .  This chapter looks at the evolution of surface pressure and how it relates to solar activity. It explores the nature of the interaction between the atmosphere at the northern and southern poles.
  34. WEATHER ORIGINATES IN THE OZONOSPHERE Takes the focus to a regional and local perspective to answer the question as to why the mid latitudes of the southern hemisphere have been colder in winter of 2016.
  35. JET STREAMS Compares and contrasts two quite different explanations for the strong winds that manifest where the troposphere and the stratosphere overlap.
  36. JET STREAMS AND CLIMATE CHANGE Looks at some great work that measures the ozone content of the air across the northern hemisphere and sets up a classification in a novel fashion, by zone of commonality rather than latitude. Relates the distribution of ozone to the occurrence of the subtropical and polar jet streams.  Zones of surprisingly uniform ozone content lie between the jets, and both pole-wards and equator-wards of the jets. Tropopause height steps down at the latitude of the jets creating marked contrasts in atmospheric density. This is a very useful and rock solid survey of great importance given the relationship between ozone and surface pressure.
  37. THE HISTORY OF THE ATMOSPHERE IN TERMS OF UPPER AIR TEMPERATURE An examination of temperature dynamics at the 10 hPa pressure surface over the poles.Critical to understanding the evolution of climate over the period of record.
  38. E.N.S.O. RE-INTERPRETED. The origin of the El Nino Southern Oscillation phenomenon and why the matter is of little consequence.

 

Here is how would I explain the Earth’s natural modes of climate change to a child!

Let us consider the Earth as a car. We are at some latitude (like being in the back or the front seat of a car). Let’s imagine we have the heater in the front of the car and a vent over the back seat. You can open and close the vent and turn it to the front to scoop in air or to the back and suck air out of the car. So, the cold air from the vent can blow straight down the back of your neck or you can turn the vent around so that it sucks air out of the car so that the warm air from the engine travels to the back of the car.

Ozone heats the air in winter creating polar cyclones that lower surface pressure at the pole attracting a flow of air from the equator. More ozone = lower surface pressure in high latitudes = wind blows more often from the equator. Less ozone= higher surface pressure at the pole= wind from equator does not come. Instead, a cold wind comes from the pole similar to what would happen if you turned the vent in the car roof so it faced forwards.

The second way in which ozone changes surface temperature is by changing cloud cover. Because ozone is mainly present in the upper air and it ascends strongly at the poles in winter it has to come down somewhere else. Where it  descends it warms the air and evaporates cloud letting the sun shine through to be absorbed by the ocean that acts like a battery because it stores energy.  Full dense cloud  curtails solar radiation by as much as 90%.

The climate varies by warming and cooling  in winter. It is in winter that we see the big changes in 1. Polar surface pressure, 2. The ozone content of the air 3. The direction of the wind and hence  the temperature at the surface.

Change can be two way, both warming and cooling.

Ozone is inextricably linked to surface pressure. The key to unlocking the cause of climate change lies in working out what can change the ozone content of the air near the poles in winter.