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about Gavin Schmidt

Gavin Schmidt is a climate modeler, working for NASA and with Columbia University.

Global Warming debate Küresel Isınma Müzakeresi

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Along with Richard Somerville (UC San Diego) and Brenda Ekwurzel (Union of Concerned Scientists), I’ll be appearing at a debate on Wednesday (March 14th) about whether Global Warming is a crisis (or not). That might have gone without notice (like most of my public talks), except that our opponents are Michael Crichton, Richard Lindzen and Philip Stott. The preliminary position statements (from me and from Philip Stott) are available on the ABCnews site. It’s sold out, but the proceedings will be broadcast on NPR (for instance, WNYC 820 AM on Friday, March 23, 2007 at 2PM) and there will be a podcast (though I don’t know if it will stream live). There’s an online poll as well for what that’s worth.

I’m quite looking forward to this, but I have to admit to conflicting thoughts. Does participating help perpetuate the idea that global warming per se is still up for debate? Is this kind of rhetorical jousting useful for clarifying issues of science that most people there will only superficially grasp? Can this be entertaining and educational? Or does it just validate the least serious opposition? Is it simply a waste of time that would be better spent blogging? ;)

I’d be interested in any thoughts people might have.


Küresel Isınma Müzakeresi

Ingilizce’den çeviren Figen Mekik

Richard Sommerville (UC San Diego) ve Brenda Ekwurzel eşliğinde (Union of Concerned Scientists-Endişeli Bilim Insanları Birliği), 14 Mart Çarşamba günü küresel ısınmanın kriz olup olmadığını tartışacağımız bir müzakereye katılacağım. Bu pek farkına varılmadan geçip gidebilirdi (benim pek çok halka açık konuşmam gibi) ama bu sefer karşı tarafta Michael Crichton, Richard Lindzen ve Phillip Stott var. Iki tarafın da tezini savunan ayrı birer yazı (ben ve Stott yazdık) ABC news sitesinde var. Müzakere’ye biletler çoktan satılmış, bitmiş. Ama müzakere hem radyoda (NPR, mesela WNYC de Cuma-23 Mart- sabahı 8:20de) yayınlanacak hem de bir podcast hazırlanıyor (ama canlı olmayacak sanırım). Internet sitelerinde bir de anket var.

Ben buna pek hevesliyim, ama bazı çelişkili düşüncelerim de var. Böyle bir müzakereye katılmak, küresel ısınmanın olup olmadığının hala tartışmaya açık olduğunu savunmak mı oluyor? Bu tip çekişmeler, oradaki insanları bilimsel konularda eğitmeye yarar mı? Bu hem eğlenceli hem de eğitici olabilir mi? Ya da ciddi bir muhalefeti geçerli kılmaya mı yarıyor? Yoksa bloglarla uğraşmaya ayıracağım zamanı buraya giderek boşa mı harcamış olacağım? ;)

Tüm fikirlerinize açığım.

Hurricane Heat Kasırga AteşiChaleur d’ouragan

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The big problem with much of the discussions about trends in hurricane activity is that the databases that everyone is working from are known to have significant inhomogeneities due to changes in observing practice and technology over the years. So it’s not surprising that a new re-analysis (Kossin et al, published yesterday) has been generating significant interest and controversy among the hurricane research community (see e.g. Prometheus or Chris Mooney). However, rather than this study being taken for what it is – a preliminary and useful attempt to make homogeneous a part of the data (1983 to 2005) – it is unfortunately being treated as if it was the definitive last word. We’ve often made the point that single papers are not generally the breakthroughs that are sometimes implied in press releases or commentary sites and this case is a good example of that.
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Cold Case vs. CSI

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If you are a follower of TV crime shows, it is likely that you’ve come across one of the CSI offshoots (CSI stands for Crime Scene Investigation) and a slightly less well known show called ‘Cold Case‘. In both these shows, difficult crimes (usually murders) are solved using the most up-to-date forensic methods and incredible detective work. However, it will be obvious to even the most jaded TV watcher that the CSI crew get to have a lot more fun with the latest gadgets and methodologies. The reason for that is clear: with a fresh crime scene there is a lot more evidence around and a lot more techniques that can be brought to bear on the problem. In a ‘Cold Case’ (where the incident happened years before), options are much more limited.

Why bring this up here? Well it illustrates nicely how paleo-climate research fits in to our understanding of current changes. Let me explain….
A partial translation of this article in Slovak is available here (courtesy Alexander Ač).
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The Physics of Climate Modelling La physique de la modélisation du climat

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This is just a pointer to a ‘Quick Study’ guide on The physics of climate modelling that appears in Physics Today this month, and to welcome anyone following through from that magazine. Feel free to post comments or questions about the article here and I’ll try and answer as many as I can.

Cet article est aussi disponible en français.

The main article is also available in Portugeuse.

AGU Hangover

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It turns out that there were almost 14,000 attendees at AGU last week, which apparently makes it the largest Earth Science meeting ever held. To be sure, not all of that is climate related – there was lots of seismology, planetary and more theoretical/small-scale stuff, but a lot of it was. At most times there were at least half a dozen sessions that I would have been interested to attend – and they were often discussing overlapping themes.

It used to be that one could go to a meeting like this and get a wide overview of the work being done much more efficiently (and speedily) than reading the journals. However, that is clearly no longer true. And of course, we can’t keep up with all the relevant journal articies in the wider field either, and so how do scientists manage?
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Fall AGU

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The Fall AGU meeting in San Francisco is always an exhilarating/exhausting (take your pick) fixture of the Earth Science calendar. This year will be no different, and since about half of us will be there, RealClimate will probably be a little quiet next week. Hopefully, we should be able to report on any highlights when we get back.

N.B. If any readers will be attending and want to say hi, I will be giving a talk on ‘Science blogging: RealClimate.org and the Global Warming debate‘ on Friday (PA53A, 13:40, MCS 309).

Update: AGU went well – lot’s of good stuff. The actual RealClimate presentation is available here – it’s pretty basic though (only 15 minutes worth)).

Inhofe’s last stand

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Part of me felt a little nostalgic yesterday watching the last Senate hearing on climate change that will be chaired by Sen. James Inhofe. It all felt very familiar and comforting in some strange way. There was the well-spoken ‘expert’ flown in from Australia (no-one available a little closer to home?), the media ‘expert’ from the think tank (plenty of those about) and a rather out-of-place geologist. There were the same talking points (CO2 leads the warming during the ice ages! the Medieval Warm Period was warm! it’s all a hoax!*) that are always brought up. These easy certainties and predictable responses are so well worn that they feel like a pair of old slippers.
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Historical climatology in Greenland

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Gavin Schmidt & Michael Mann

Extending the instrumental record of climate beyond the late 19th Century when many of the national weather centers were first started is an important, difficult and undervalued task. It often is more akin to historical detective work than to climatology and can involve long searches in dusty archives, the ability to read archaic scripts and handwriting, and even Latin translations (for instance, when going through the archives of the Paris Observatory) (sounds like a recent bestseller, only less lucrative, no?).
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The sky IS falling Le ciel nous tombe vraiment sur la tête

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A timely perspective article in Science this week addresses the issues of upper atmosphere change. ‘Upper’ atmosphere here is the stratosphere up to the ionosphere (~20 to 300 km). Laštovička et al point out that cooling trends are exactly as predicted by increasing greenhouse gas trends, and that the increase in density that this implies is causing various ionspheric layers to ‘fall’. This was highlighted a few years back by Jarvis et al (1998) and in New Scientist in 1999 (and I apologise for stealing their headline!).

The changes in the figure are related to the cooling seen in the lower stratospheric MSU-4 records (UAH or RSS), but the changes there (~ 15-20 km) are predominantly due to ozone depletion. The higher up one goes, the more important the CO2 related cooling is. It’s interesting to note that significant solar forcing would have exactly the opposite effect (it would cause a warming) – yet another reason to doubt that solar forcing is a significant factor in recent decades.

Update: The best explanation for the cooling trends can be found on ESPERE (alternative site), in particular, figure 3 (alt. version).


Traduit par Etienne Pesnelle
Dans le numéro de cette semaine de Science, un article opportun de mise en perspective traite des problèmes du changement de l’atmosphère supérieure. Ladite atmosphère “supérieure” consiste en la stratosphère jusqu’à l’ionosphère (~20 à 300 km). Laštovicka et al soulignent que la tendance au refroidissement est exactement telle que prédite par la tendance à la hausse des gaz à effet de serre, et que l’accroissement de densité que cela implique est en train de provoquer la “chute” de différentes couches de la ionosphère. Cela a été mis en exergue il y a quelques années par Jarvis et al. (1998) et dans New Scientist en 1999 (et je m’excuse de leur avoir volé le titre de leur article!).

Les changements dans le graphique sont liés au refroidissement constaté dans les enregistrements MSU-4 de la basse stratosphère (que ce soit ceux provenant des bases de données UAH ou RSS), mais les changements à ces altitudes (~ 15-20 km) sont principalement dûs à la raréfaction de l’ozone. Plus on monte, plus le refroidissement dû au CO2 est important. Il est intéressant de noter qu’un forçage solaire significatif aurait exactement l’effet inverse (il provoquerait un réchauffement) – encore une autre raison de douter que le forçage solaire est un facteur significatif [du réchauffement climatique] des dernières décennies.

Mise à jour : la meilleure explication des tendances au refroidissement peut être trouvée sur ESPERE, en particulier la figure 3.

English vineyards again….

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Readers may recall a thorough examination of the history of English wine here a few months ago – chiefly because the subject tends to come up as a contrarian climate talking point every now and again. The bottom line from that post was that the English wine industry is currently thriving and has a geographical extent and quality levels that are unprecedented in recorded history. So whether vineyards are a good proxy for climate or not, you certainly can’t use the supposed lack of present day English vineyards in any serious discussion about climate….

So along comes this quote today (promoting Fred Singer’s latest turnaround) (my emphasis):

“The Romans wrote about growing wine grapes in Britain in the first century,” says Avery, “and then it got too cold during the Dark Ages. Ancient tax records show the Britons grew their own wine grapes in the 11th century, during the Medieval Warming, and then it got too cold during the Little Ice Age. It isn’t yet warm enough for wine grapes in today’s Britain. Wine grapes are among the most accurate and sensitive indicators of temperature and they are telling us about a cycle. They also indicate that today’s warming is not unprecedented.”

Hmmm…. so where did that bottle of Chapel Down in my fridge come from? (thanks Dad!) Or the winners of the ‘Best Sparkling Wine’ for the last two years at the International Wine and Spirit Competition? This is of course a trivial point, but it demonstrates (once again) that our contrarian friends don’t even have a semblence of a desire to get it right. The lure of a talking point clearly trumps the desire for accuracy.

In vino veritas (though not in this case).

Update: We had the Chapel Down Flint Dry last night. Fruity, hints of apple and pear and one of better whites I’ve had in a while. Highly recommended!