What happens to Steig et al's warming when you divide Antarctica into two distinct climate zones?

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
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.

antarctic_climate_zones1

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.

Going back to basic climatology one can recall the Köppen climate classification system. Antarctica has been classified as EF

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.
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
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:

http://noconsensus.wordpress.com/2009/02/15/aws-gridded-reconstruction/

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.

Spatially Weighted Antarctic Temperatures – No Peninsula

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.

nop-id-recon-total-trend

Figure 1

Spatial trends with clipping region shown in black Figure 2.

Figure 2

Figure 2

As I’ve shown before, the trends from 1967 onward.

Figure 3

Figure 3

Spatial distribution 1967 onward.

Figure 4

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.

trend-table

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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Bill Illis
April 18, 2009 3:52 pm

Antartica and South America were more-or-less still connected even 40 million years ago. I believe this animation from the McMurdo base has it right based on the locations of the mid-oceanic ridges.
http://www.exploratorium.edu/origins/antarctica/ideas/gondwana2.html
There are volcanoes all the way from the tip of the Peninsula to west of the Ross ice-shelf.
http://www.volcano.si.edu/world/region.cfm?rnum=19&rpage=list

enduser
April 18, 2009 4:00 pm

“Smokey When you just follow the link you get a location map that is dated 2003, you have to actually click ‘Show Image’ button to get the image for the date 10 April 2009. It is confusing, and had me going to.”
What am I missing here?
Smokey, it had you going?
I still do not understand why NSIDC shows a 1994 picture and labels it April 10, 2009.
Seriously, If I have made a mistake here, please tell me what it is. Original post follows:
I notice at NSIDC that the photo for Wilkins, 10 April 2009 ( MODIS visible) is exactly the same as the photo for AVHRR image (visible) 20 February 1994.
The very same photo. Please confirm that my eyes are not deceiving me.
http://nsidc.org/data/iceshelves_images/wilkins.html

janama
April 18, 2009 4:07 pm

James Griffin (13:21:22) :
the peninsula is part of the Pacific ring of fire so it has many active and extinct volcanoes as does Chile and Bolivia to the north.
In fact no one actually knows how many undersea volcanoes exist in the area because no one has looked.
The South Sandwich islands, Decpetion, Bridgeman, Paulet and Penguin islands are all in the area and are active.
Reply: Deception Island is a beautiful place. I’ve been there. Ready to eat boiled shrimp sometimes wash up on the shore. ~ charles the moderator

timetochooseagain
April 18, 2009 4:17 pm

Lucy Skywalker (14:38:35) It would be pretty silly to say “Antarctica is rapidly becoming a desert when it actually already is one!

janama
April 18, 2009 4:19 pm

There are around 35 volcanoes in antarctica.
here’s the ones I managed to find in the area.
http://users.tpg.com.au/johnsay1/Stuff/volcanoes.jpg

janama
April 18, 2009 4:21 pm

Charles – there must be undersea volcanoes if the shrimp come up boiled already 🙂
Reply:The entire Island is a volcano. You sail into the caldera through a collapsed wall. ~ charles the moderator

EricH
April 18, 2009 4:33 pm

Well spotted Enduser.
It makes you wonder just how many old photographs there are out there that are being recycled time after time claiming each time to be the latest, up to date, information.
Enjoy.

Philip_B
April 18, 2009 5:47 pm

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.
Precipitation would be a good proxy for which dominates where. The precipitation map above shows high precipitation not only on the Peninsula but also along a large part of the edge of East Antarctica.
If you want to separate Antarctica into 2 climate zones then I would include the parts of East Antarctica with precipitation over 600mm in the polar maritime zone. IMHO of course.

kuhnkat
April 18, 2009 5:50 pm

Britannic no-see-um,
those puzzle pieces really look like they fit well, that is, until you realize that you need to include the continental shelf areas for this type of fitting game.
Purchase a cheap cardboard globe that shows shelf area, cut out the pieces, and see how well they fit that-a-way!! Doesn’t disprove anything as there could be many stretching/compression areas not easily identified, but, shows it just ain’t that simple!!

enduser
April 18, 2009 7:15 pm

Steve Keohane (15:48:56) :
“Thanks again jeff and Anthony, but I doubt there this obviously valid premise cannot be implimented because, as you say:
“2)Treatment of the Antarctic peninsula climate zone as an outlier likely ruins the premise of the study in the first place.”
enduser (12:09:06) Re: “I notice at NSIDC that the photo for Wilkins, 10 April 2009 ( MODIS visible) is exactly the same as the photo for AVHRR image (visible) 20 February 1994.” This does not seem to be the case. I captured the April 10 2009 and the February 20 1994 images. I scaled the 2009 image as closely as possible to the 1994 image (which I increased the contrast on), and labeled them respectively. See here: http://i44.tinypic.com/eknx5j.jpg
Smokey When you just follow the link you get a location map that is dated 2003, you have to actually click ‘Show Image’ button to get the image for the date 10 April 2009. It is confusing, and had me going to”
REPLY:
The picture that is retrieved for AVHRR visible image 20 February 1994 now is NOT the same picture that I retrieved earlier today! SOMETHING IS NOT RIGHT HERE!
The picture that I retrieved earlier today for 20 February has been changed. I saved it, and have it available on my HD.

enduser
April 18, 2009 7:28 pm

C,mon somebody has to have these pictures archived on their computers.
If I am telling the truth (and I am), then this is very serious.

kent
April 18, 2009 8:22 pm

The summer/winter thermal graphs of Antarctica with temperature gradiants, gave me a picture of just how far cooling extended in the winter. Funny because I had just started wondering how many square Km of open Antarctic waters were exposed to cooling air and I see it here. Thanks for that.
The whole story about polar contributions to climate change needs to include the cooling of sea water.

Mike Bryant
April 18, 2009 8:26 pm

Sorry enduser,
When I checked what you said it looked OK to me…
Mike Bryant

Mike Bryant
April 18, 2009 8:31 pm

janama (16:21:25) :
Charles – there must be undersea volcanoes if the shrimp come up boiled already 🙂
Reply:The entire Island is a volcano. You sail into the caldera through a collapsed wall. ~ charles the moderator
You’re kidding right Charles? Is there a cocktail sauce fountain and a beer fountain there too, or do you bring your own?

Bill Illis
April 18, 2009 8:37 pm

If you are looking for Wilkins satellite pics, this is the NSIDC archive, with some pics going back to 1989. The Feb 20th one and the April 10th one are in there.
ftp://sidads.colorado.edu/pub/DATASETS/ICESHELVES/wilkins/

Jim F
April 18, 2009 8:51 pm

Congratualtions, Anthony? (it was you who posted the climate zone info?). this is really good thinking, and based on the evidence you presented, probably a very useful and realistic revision of the climatic classification of Antarctica. I think you should spruce it up and submit it to an appropriate scientific magazine or body for consideration.
I had been thinking about writing something along similar but different lines. This just makes what I want to say easier. What we have in Ant. is two (at least) areas that are essentially different. Temperature data from one has no “statistical” correlation with the other(s) except by coincidence.
Mining geologists have wrestled with similar issues for eons. They have a limited amount of assay data from drill holes and other sampling of a mineralized body. Now they have to make an “ore reserve” estimate in order to determine whether there is an economically feasible mining operation, and if so, then make a mining plan to direct the actual drilling/blasting/digging of rock, some of which gets milled, the rest gets dumped. Steig et al. were, in a sense, doing the “ore reserve”.
If the ore deposit were relatively homogeneous, then one can reasonably infer that an assay here is related to one over there, and one can infer the ore content of the rock between the two (here is 1 ounce, there is 2 ounces. Halfway between should be 1.5 ounces, no?) Too often, deposits are not homogeneous. Geostatisticians have dealt with this issue for many years, and have developed techniques to cope with two or more populations of sample results.
Basically, what they would do is to segregate the data for the high-grade vein deposit (West Ant.) from that for the much larger, more homogeneous porphyry copper deposit (East Ant.) and make the calculations – and ultimately – ore reserve estimates (temperature blocks/areas or trends, if you will) for the two areas independently.
An approach to the “temperature trends” of the Antarctic following this school of statistics would have strong scientific underpinnings. Mixing the two, as both Steig and Id have done, simply is statistically invalid, and most likely, wrong.

April 19, 2009 12:07 am

The idea of applying Steig’s method to America is interesting, and might be good for a laugh. Australia is similar in some aspects to Antarctica, size, interior different from the perimeter, etc, and might also be a good candidate.

Rhys Jaggar
April 19, 2009 5:40 am

I have to laugh at calling Antarctica ‘one climate zone’.
That’s like linking Alaska to California – when everyone knows that their climates aren’t linked closely.
How about Britain to the Balkans?
And Chukotka to inner Siberia?
The reason most work is done on the Antarctic peninsula is:
i. It’s accessible.
ii. It’s less cold and frigid.
iii. It shows what people want it to show.

April 19, 2009 5:46 am

Jim F,
Mixing the two, as both Steig and Id have done,
You’ll notice I removed the peninsula in the above reconstruction to analyze temp trends. Ive done this in at least two other reconstructions as well. Also, Jeff C and I have provided several alternative reconstructions all based on improved localization of the temperature data.
I agree Anthony’s suggestion is quite valid and at the same time I don’t agree that it is statistically invalid to consider both regions in total trend. If you want the temperature trend of the earth you don’t cut off bits. It’s important that the contribution of the different areas are properly weighted though.
I think it would be hard for someone to argue that a reconstruction excluding the ocean controlled temperatures of the peninsula is invalid, so on that point we agree.

enduser
April 19, 2009 6:36 am

Well, Last night I was ready to claim grand conspiracy, but having slept on it, and looking at the NSIDC site again, I can concede that the most likely thing that happened is that I selected Feb 20, 1994 on the AVHRR menu and accidentally hit the SHOW IMAGE tab for MODIS which was already set by default for Apr 10, 2009.
Thank you for taking the time to correct me on this, I will go and hang my head in shame for a while….
Unless…. [eyes narrowing and darting back and forth] You are ALL in on it! In which case I must go and make a tin foil hat.

Mike Bryant
April 19, 2009 7:13 am

Alright guys… nice work on that image thing… enduser almost caught us…

Mike Bryant
April 19, 2009 7:15 am

“Mike McMillan (00:07:22) :
The idea of applying Steig’s method to America is interesting, and might be good for a laugh. Australia is similar in some aspects to Antarctica, size, interior different from the perimeter, etc, and might also be a good candidate.”
I think BOM already has that covered.
Mike

Mike Bryant
April 19, 2009 9:33 am

It seems odd that the coldest temperatures in the Antarctic are offset to the East of the South Pole, and the Beaufort Gyre in the Arctic is offset to the West of the North Pole. It’s a nice little bit of symmetry there, but could it mean anything at all?

Jim F
April 19, 2009 10:00 am

Jeff Id: Sorry, I didn’t mean to tar you with the brush I would use for Steig. I think I had in mind and was referring to some earlier work you had done on Steig’s data, where you were folding all the data together. I appreciate too that above you have separated the data sets. My apologies for sloppy writing.
I agree that to get an idea/estimation of the Earth’s climate trends and variability (or maybe Antarctica’s) one would use all the data. But to calculate an estimated temperature at point x, 200 miles thataway from measurements at points y and z, which is what Steig is doing, I think it wrong to mix the data if they are indeed different. The much higher temperatures measured on the Peninsula are relatively localized; they don’t have any effect on the temperatures way up on that mountain of ice called East Ant. Yet Steig’s approach smears a component of those warm results all across the continent. It’s no wonder Antarctica is heating up! 😉

Brian Dodge
April 19, 2009 11:37 am

According to the World Climates link”E – Cold Climates … Only about four months of the year have above freezing temperatures.” but according to Connelly’s map even the summertime temperatures are below freezing for anything south of the tip of the Antarctic Peninsula.
If we’re going to reclassify, shouldn’t there be a primary category F (temperatures below freezing almost year round) with subgroups M (maritime-high rainfall) and D(dry continental interior). These zones might also be applied to Greenland, depending on the precipitation pattern; anyone know when & how much snow falls on interior Greenland?

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