A week ago I made this comment to Jeff Id on The Air Vent regarding his reconstruction of the Steig et al Antarctic temperature trends paper. The idea was to treat Antarctica as two distinct climate zones. I should point out that this idea has not been accepted yet, but there are some good reasons to consider it.
Köppen world climate classification
As seen in the map above, currently Antarctica is classified per the Köppen climate classification system entirely as EF, or “Ice Cap”. But here is what it might look like if the peninsula was classified differently.
I’ve made some enhancements with inline images and links to my original comment on The Air Vent for WUWT readers:
Jeff, in looking at your output maps above something occurred to me about the climate the Antarctic peninsula.
The biggest problem I see with Antarctica in either yours or Steig’s reconstructions is the treatment of the continent as a single climate zone, when in fact the climate of the peninsula has a significantly different set of temperature and precipitation norms than the majority of the main continent.
EF =Ice Cap Climate – All twelve months have average temperatures below 0 °C (32°F) There has been some discussion that the Aleutian peninsula might be better served if newly classified as EM (Maritime Polar) This would separate relatively mild marine locations such as Ushuaia, Argentina and the outer Aleutian Islands like Unalaska The climate of Unalaska from the colder, continental climates. The mean annual temperature for Unalaska is about 38 °F (3.4 °C), being about 30°F (−1.1°C) in January and about 52°F (11.1°C) in August. With about 250 rainy days a year.
Contrast that to interior Alaska temperatures which are not moderated by the presence of the sea. Fairbanks for example has an mean annual temperature for Fairbanks is 26.9°F (-2.8°C) and with 106 rainy days.
Using the Unalaska to Fairbanks comparison, the Antarctic peninsula would be a candidate for this new “Maritime Polar” (EM) classification IMHO.
In support of that, here is a seasonal temperature map submitted to Wikipedia by Stoat’s William Connelly:
Antarctic surface temperature from ECMWF (era40) reanalyses, 1979-2001.
Note how in winter the Antarctic peninsula is completely at the other end of the temperature scale from the interior just as we see in the Unalaska to Fairbanks comparison. In the summer, the effect is less, but the Antarctic peninsula agrees mostly with the sea temperature band surrounding the Antarctic continent.
Another piece of support evidence that the Antarctic peninsula climate is vastly different than the interior continent is precipitation, the other half of the Köppen climate classification system.
Here is a map of Antarctic precipitation:
Map of average annual precipitation (liquid equivalent, mm) on Antarctica
Note once again that in terms of precipitation the Antarctic peninsula climate is also vastly different than the interior continent. It seems the Antarctic peninsula is an outlier when compared to the rest of the continent. The peninsula gets 400-600+ mm of precip while the interior gets 0-100mm.
As Köppen understood, places that are connected geographically and politically aren’t always connected by a common climate. Note another factor that you pointed out in this article:
Note that we have the majority of weather stations in Antarctica on the peninsula in your grid cell C, a total of 11. No other place in Antarctica comes close in the number of weather stations. Further, that grid cell also happens to be the one where the climate diverges from the interior of Antarctica the most.
So why is the obviously different Antarctic peninsula climatic zone being considered in the Steig study at all? The answers are: 1) it is connected geographically to the continent so that when saying “Antarctica is warming” the statement is true. 2)Treatment of the Antarctic peninsula climate zone as an outlier likely ruins the premise of the study in the first place.
Of course the counter argument would be that: “Antarctica is classified as one climate zone, thus our analysis in robust” but my counter argument would be that we could also likely find the same results from a study of the USA if we had the majority density of weather stations in the study based in the Florida keys and south Florida, with a remainder around the coastal cities of the USA and maybe a few in the interior. Could we accurately derive the climate trend of the USA from such and arrangement? Me thinks not.
To test this, I’d like to see what happens when the interior and the peninsula are are treated as separate climate zones. You could pick a delineation line right at the base, or go further out the peninsula, I doubt it would make much difference given the station weighting. Produce separate outputs showing the continent versus the peninsula.
I’ll bet the results will be obvious and telling.
Well, Jeff obliged and did the analysis I suggested. I thank him for that. While the decadal temperature trend does switch from positive to negative, there is some new information that has emerged about the RegEM analysis.
Posted by Jeff Id “The Air Vent” on April 18, 2009
From this post and others I’ve determined that the temperature trend in the RegEM versioins of the Antarctic are not entirely created by smearing of the peninsula station’s data.
In order to interpret the RegEM results from the previous peninsula free reconstruction, we need to see a baseline reasonable reconstruction without the peninsula. These trends are based entirely on the surface station data. I saw several questions on WUWT about the improved accuracy of satellite temperatures. The satellite temperatures in this paper are of a different type than UAH or RSS use and these are affected substantially by clouds. The result is a much noisier and less trustworthy dataset than surface measurements.
In my opinion this sort of thing is about the best we can do in determining a total trend for the Antarctic over this timeframe. There are a few tweaks which might help but beyond that we have to accept that we don’t know any better than this method shows.
Now removing the peninsula does have basis in science because the ultra thin strip of land is primarily dependent on ocean temperatures and currents. It will be seen as cherry picking because I’ve clipped the part of the Antarctic warming the most. Before TCO or someone points out that I wouldn’t clip it if it didn’t have warming, keep in mind that I show it both with and without the peninsula and I make no claim that clipping the peninsula is the preferred method. It does make some sense though.
First the full trend.
Figure 1
Spatial trends with clipping region shown in black Figure 2.
Figure 2
As I’ve shown before, the trends from 1967 onward.
Figure 3
Spatial distribution 1967 onward.
Figure 4
If I’ve learned anything from all these plots, it’s that the Antarctic isn’t warming at 0.12 +/- 0.7 C/decade. It just isn’t. The actual trend is much lower than that and since 1967 it has even dropped a little across the continent.
Now from the other reconstructions we have the following.
Compared to the 0.12 that Steig et al. claims the real trends are pretty low. When the peninsula is removed in the properly weighted reconstruction presented here the trend drops by(0.52-.39)/.52 x100 =25%. This represents a very large contribution to the average simply because this tiny area has shown so much warming.It doesn’t seem reasonable to adjust the continent upward 25% based on this little strip of land.
Surprisingly, in RegEM the trend changes by an similar amount (0.108-0.074).0.08 x100 =31%. This is impressively similar to me as many have speculated that the positive trend in RegEM is created by smearing of peninsula trends. In my spatial reconstruction above, there is no smearing of the peninsula trend at all and there is a 25% trend drop when the peninsula is removed. This means to me that the RegEM high positive trend is not wholly created by the peninsula. Also, this does not mean the trends aren’t smeared by RegEM, they are.
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jorgekafkazar
April 19, 2009 1:02 pm
Now I’m wondering what the trend would be if the volcanic areas were separated from the analysis. The result can probably be guessed by inspection…
pft
April 19, 2009 4:31 pm
Philip_B (17:47:48) : “Antarctic weather is dominated by 2 different effects. One is the intense low pressure systems that constantly circle Antartica. The other is the very cold, very dry katabatic winds that blow out from the interior of Antarctica.”
These cold dry katabatic winds flow down from the higher elevations, 2 to 3 miles to the surface and actually warm as they descend, a source of warming at the surface. http://profhorn.aos.wisc.edu/wxwise/AckermanKnox/chap12/katabatic_winds.html
Jim F
April 19, 2009 5:05 pm
jorgekafkazar re volcanism. True, there will be higher heat flow in parts of the volcanic belt in W. Ant. The effects however should be localized; there is such a stupendous amount of cold water impinging on this belt that there will probably be no measurable change in regional oceanic temperatures. Locally, like in a noted caldera, hot springs/lava flows may boil your shrimp dinner for you.
However, other effects may be noticeable. Hot magma rises, forcing up rocks above it. This could dislodge chunks of ice sheets that apparently are anchored to rocks that the ice has depressed below sea level. Maybe some portions of ice will become dislodged and slide off the building mound. Similarly, lava and hot springs might melt those ice-rock joins, letting the ice float free.
Much depends on time, first (these are generally slow processes) and second, the composition of the volcanism. Basalts don’t give much explosive activity (the magma has little silica in it, and so is relatively fluid). Andesitic to rhyolitic volcanism – much more siliceous – can result in explosive events, which might blast out a chunk of ice of considerable proportions.
Philip_B
April 19, 2009 5:30 pm
pft, what you say is true. However, to be warming toward the coast would require the lapse rate of the katabatic winds to be greater than temperature differential due to altitude, and that seems not to be the case.
Ie, katabatic winds are colder than otherwise prevailing temperatures toward the coast.
I just lost the link and my battery is about to run out. So you will have to take my word.
Alan Chappell
April 20, 2009 9:19 am
Not only has this site some fantastic photos but lots and lots of data, volcanoes, volcanoes and more volcanoes, http://www.thewe.cc/weplanet/poles/antarcti/mastvolcanoe.html I would think that any serious study of the volcanic activity on the Antarctic Peninsula would show that it could not be part of any climate study of the Antarctic, think a little, 2km offshore and 2,800mt, water depth and boiling water on the ocean surface could not have any effect on the local climate [one of several] cauldrons off the Peninsula.
gary gulrud
April 20, 2009 9:40 am
Nice articulation of an unexamined assumption.
Leon Palmer
April 20, 2009 11:29 am
More (unitentional) support for this thesis: http://www.newscientist.com/article/dn16988-why-antarctic-ice-is-growing-despite-global-warming.html
pointing out that the antarctic peninsula isn’t like the rest of Antarctica…
“In a new study, Turner and colleagues show how the ozone hole has changed weather patterns around Antarctica. These changes have drawn in warm air over the Antarctic Peninsula in West Antarctica and cooled the air above East Antarctica.”
I like the ending “”Over the next 50 to 100 years, the ozone hole will heal,” says Turner. “At the same time, greenhouse gases will rise. In next decade or so we should see sea ice plateauing and then decreasing massively if greenhouse gases continue to increase.”
I thought CO2/AGW caused ozone depletion, so how is this healing (sometime in the misty future) gonna happen?
pft
April 20, 2009 3:21 pm
“Philip_B (17:30:44) :
pft, what you say is true. However, to be warming toward the coast would require the lapse rate of the katabatic winds to be greater than temperature differential due to altitude, and that seems not to be the case.”
Phillip, The followng paper is available online, no time to find link:
“Climatology of katabatic winds in the McMurdo dry valleys,
southern Victoria Land, Antarctica, Thomas H. Nylen and Andrew G. Fountain Department of Geology and Department of Geography, Portland State University, Portland, Oregon, USA, Peter T. Doran
Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois, USA
Received 1 July 2003; revised 16 October 2003; accepted 3 December 2003; published 14 February 2004.
[1] Katabatic winds dramatically affect the climate of the McMurdo dry valleys, Antarctica. Winter wind events can increase local air temperatures by 30C. The frequency of katabatic winds largely controls winter (June to August) temperatures, increasing 1C per 1% increase in katabatic frequency, and it overwhelms the effect of topographic
elevation (lapse rate). Summer katabatic winds are important, but their influence on summer temperature is less. The spatial distribution of katabatic winds varies significantly. Winter events increase by 14% for every 10 km up valley toward the ice sheet, and summer events increase by 3%. The spatial distribution of katabatic frequency seems to be partly controlled by inversions………..Although the onset and termination of the katabatic winds are typically abrupt, elevated air temperatures remain for days afterward. We estimate that current frequencies of katabatic winds increase annual average temperatures by 0.7 to 2.2C, depending on location. Seasonally, they increase (decrease) winter average temperatures (relative humidity) by 0.8 to 4.2 (1.8 to 8.5%) and summer
temperatures by 0.1 to 0.4C (0.9% to 4.1%). Long-term changes of dry valley air temperatures cannot be understood without knowledge of changes in katabatic.”
The study and effect was observed near the coast. http://en.wikipedia.org/wiki/File:Mcmurdo_sound_USGS_map.jpg
SteveSadlov
April 20, 2009 3:25 pm
The Climate of the Peninsula is akin to that of the Aleutian Islands, or, the northern Norwegian Sea coast of Norway. It is correct to split it from the main land mass.
George E. Smith
April 20, 2009 5:48 pm
So the total climate temperature range on earth goes from 72F to -36F; a mere 108F total range.
A really great classification system given that the actual measured range can be from +130F to -140 F, or +60C to -90C or 150 C (270F).
And just a glance at the color map demonstrates clearly why it isn’t nice to ignore the Nyquist Sampling Criterion.
So I guess it is nice to to have a system for describinh the weather on the nightly news; but anybody who thinks +72 F is hot is just plain nuts. I think it was around 90 today out in our parking lot; and it didn’t seem the boiling cauldron people think.
The warmth I could feel was the direct IR radiation from the blacktop parking lot, and my lungs don’t care for the vertical hot air currents; but I’m supersensitive to that; but no way I would describe it as hot.
George
George E. Smith
April 20, 2009 5:49 pm
make that +140 to -130. F
Philip_B
April 20, 2009 5:50 pm
pft, the warming effect of katabatic in dry valleys appears to be a local phenomena and generally katabatic winds in Antarctica are cold winds, ie colder than the otherwise prevailing temperatures. http://en.wikipedia.org/wiki/Katabatic_wind
Although, it does raise the question that if katabatic winds can produce substantial differences in temperatures as a result of local topography, then siting of the small number of, East Antarctica in particular, weather stations may well result in measuring trends in a local phenomena (katabatic winds) rather than ‘global’ climate effects.
pft
April 21, 2009 3:46 pm
Philip_B (17:50:04) :
Katabatic winds are heated adiabatically which is why the air and the valleys are dry. They may be cold, but they still tend to end up warmer than prevailing temperatures when they are most intense, especially in the winter. It is a local effect only to the extent that katabatic winds are limited by topography. Any short term warming may be a result of variations in the intensity of these winds from year to year, especially if weather stations happen to be located nearby.
Anyways, here is that paper. http://www.glaciers.pdx.edu/fountain/MyPapers/NylenEtAl2004.pdf
Now I’m wondering what the trend would be if the volcanic areas were separated from the analysis. The result can probably be guessed by inspection…
Philip_B (17:47:48) :
“Antarctic weather is dominated by 2 different effects. One is the intense low pressure systems that constantly circle Antartica. The other is the very cold, very dry katabatic winds that blow out from the interior of Antarctica.”
These cold dry katabatic winds flow down from the higher elevations, 2 to 3 miles to the surface and actually warm as they descend, a source of warming at the surface.
http://profhorn.aos.wisc.edu/wxwise/AckermanKnox/chap12/katabatic_winds.html
jorgekafkazar re volcanism. True, there will be higher heat flow in parts of the volcanic belt in W. Ant. The effects however should be localized; there is such a stupendous amount of cold water impinging on this belt that there will probably be no measurable change in regional oceanic temperatures. Locally, like in a noted caldera, hot springs/lava flows may boil your shrimp dinner for you.
However, other effects may be noticeable. Hot magma rises, forcing up rocks above it. This could dislodge chunks of ice sheets that apparently are anchored to rocks that the ice has depressed below sea level. Maybe some portions of ice will become dislodged and slide off the building mound. Similarly, lava and hot springs might melt those ice-rock joins, letting the ice float free.
Much depends on time, first (these are generally slow processes) and second, the composition of the volcanism. Basalts don’t give much explosive activity (the magma has little silica in it, and so is relatively fluid). Andesitic to rhyolitic volcanism – much more siliceous – can result in explosive events, which might blast out a chunk of ice of considerable proportions.
pft, what you say is true. However, to be warming toward the coast would require the lapse rate of the katabatic winds to be greater than temperature differential due to altitude, and that seems not to be the case.
Ie, katabatic winds are colder than otherwise prevailing temperatures toward the coast.
I just lost the link and my battery is about to run out. So you will have to take my word.
Not only has this site some fantastic photos but lots and lots of data, volcanoes, volcanoes and more volcanoes, http://www.thewe.cc/weplanet/poles/antarcti/mastvolcanoe.html I would think that any serious study of the volcanic activity on the Antarctic Peninsula would show that it could not be part of any climate study of the Antarctic, think a little, 2km offshore and 2,800mt, water depth and boiling water on the ocean surface could not have any effect on the local climate [one of several] cauldrons off the Peninsula.
Nice articulation of an unexamined assumption.
More (unitentional) support for this thesis:
http://www.newscientist.com/article/dn16988-why-antarctic-ice-is-growing-despite-global-warming.html
pointing out that the antarctic peninsula isn’t like the rest of Antarctica…
“In a new study, Turner and colleagues show how the ozone hole has changed weather patterns around Antarctica. These changes have drawn in warm air over the Antarctic Peninsula in West Antarctica and cooled the air above East Antarctica.”
I like the ending “”Over the next 50 to 100 years, the ozone hole will heal,” says Turner. “At the same time, greenhouse gases will rise. In next decade or so we should see sea ice plateauing and then decreasing massively if greenhouse gases continue to increase.”
I thought CO2/AGW caused ozone depletion, so how is this healing (sometime in the misty future) gonna happen?
“Philip_B (17:30:44) :
pft, what you say is true. However, to be warming toward the coast would require the lapse rate of the katabatic winds to be greater than temperature differential due to altitude, and that seems not to be the case.”
Phillip, The followng paper is available online, no time to find link:
“Climatology of katabatic winds in the McMurdo dry valleys,
southern Victoria Land, Antarctica, Thomas H. Nylen and Andrew G. Fountain Department of Geology and Department of Geography, Portland State University, Portland, Oregon, USA, Peter T. Doran
Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois, USA
Received 1 July 2003; revised 16 October 2003; accepted 3 December 2003; published 14 February 2004.
[1] Katabatic winds dramatically affect the climate of the McMurdo dry valleys, Antarctica. Winter wind events can increase local air temperatures by 30C. The frequency of katabatic winds largely controls winter (June to August) temperatures, increasing 1C per 1% increase in katabatic frequency, and it overwhelms the effect of topographic
elevation (lapse rate). Summer katabatic winds are important, but their influence on summer temperature is less. The spatial distribution of katabatic winds varies significantly. Winter events increase by 14% for every 10 km up valley toward the ice sheet, and summer events increase by 3%. The spatial distribution of katabatic frequency seems to be partly controlled by inversions………..Although the onset and termination of the katabatic winds are typically abrupt, elevated air temperatures remain for days afterward. We estimate that current frequencies of katabatic winds increase annual average temperatures by 0.7 to 2.2C, depending on location. Seasonally, they increase (decrease) winter average temperatures (relative humidity) by 0.8 to 4.2 (1.8 to 8.5%) and summer
temperatures by 0.1 to 0.4C (0.9% to 4.1%). Long-term changes of dry valley air temperatures cannot be understood without knowledge of changes in katabatic.”
The study and effect was observed near the coast.
http://en.wikipedia.org/wiki/File:Mcmurdo_sound_USGS_map.jpg
The Climate of the Peninsula is akin to that of the Aleutian Islands, or, the northern Norwegian Sea coast of Norway. It is correct to split it from the main land mass.
So the total climate temperature range on earth goes from 72F to -36F; a mere 108F total range.
A really great classification system given that the actual measured range can be from +130F to -140 F, or +60C to -90C or 150 C (270F).
And just a glance at the color map demonstrates clearly why it isn’t nice to ignore the Nyquist Sampling Criterion.
So I guess it is nice to to have a system for describinh the weather on the nightly news; but anybody who thinks +72 F is hot is just plain nuts. I think it was around 90 today out in our parking lot; and it didn’t seem the boiling cauldron people think.
The warmth I could feel was the direct IR radiation from the blacktop parking lot, and my lungs don’t care for the vertical hot air currents; but I’m supersensitive to that; but no way I would describe it as hot.
George
make that +140 to -130. F
pft, the warming effect of katabatic in dry valleys appears to be a local phenomena and generally katabatic winds in Antarctica are cold winds, ie colder than the otherwise prevailing temperatures.
http://en.wikipedia.org/wiki/Katabatic_wind
Although, it does raise the question that if katabatic winds can produce substantial differences in temperatures as a result of local topography, then siting of the small number of, East Antarctica in particular, weather stations may well result in measuring trends in a local phenomena (katabatic winds) rather than ‘global’ climate effects.
Philip_B (17:50:04) :
Katabatic winds are heated adiabatically which is why the air and the valleys are dry. They may be cold, but they still tend to end up warmer than prevailing temperatures when they are most intense, especially in the winter. It is a local effect only to the extent that katabatic winds are limited by topography. Any short term warming may be a result of variations in the intensity of these winds from year to year, especially if weather stations happen to be located nearby.
Anyways, here is that paper.
http://www.glaciers.pdx.edu/fountain/MyPapers/NylenEtAl2004.pdf