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Moberg et al: Highly variable Northern Hemisphere temperatures?

15 Feb 2005 by group

Translations: (Français)

by William Connolley and Eric Steig

The 10th Feb edition of Nature has a nice paper “Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data” by Anders Moberg, DM. Sonechkin, K Holmgren, NM Datsenko, & W Karlin (doi:10.1038/nature03265). This paper takes a novel approach to the problem of reconstructing past temperatures from paleoclimate proxy data. A key result is a reconstruction showing more century-scale variability in mean Northern Hemisphere temperatures than is shown in previous reconstructions. This result will undoubtedly lead to much discussion and further debate over the validity of previous work. The result, though, does not fundamentally change one of the most discussed aspects of that previous work: temperatures since 1990 still appear to be the warmest in the last 2000 years.

[Read more…] about Moberg et al: Highly variable Northern Hemisphere temperatures?

Filed Under: Climate Science, Instrumental Record, Paleoclimate

Exeter conference: Avoiding Dangerous Climate Change

7 Feb 2005 by group

Translations: (Français)

The conference last week in Exeter on “Avoiding Dangerous Climate Change” grew out of a speech by UK Prime Minister Tony Blair. He asked “What level of greenhouse gases in the atmosphere is self-evidently too much?” and “What options do we have to avoid such levels?”. The first question is very interesting, but also very difficult. As Roger Pielke has noted the conference organisers actually choose three “key questions”:

  1. For different levels of climate change what are the key impacts, for different regions and sectors, and for the world as a whole?
  2. What would such levels of climate change imply in terms of greenhouse gas stabilisation concentrations and emission pathways required to achieve such levels?
  3. What technological options are there for achieving stabilisation of greenhouse gases at different stabilisation concentrations in the atmosphere, taking into account costs and uncertainties?

It is worth thinking about the difference between the initial aim and the “key questions” chosen. Question 1 is essentially IPCC WGII impacts); question 2 is firmly WGI (how-much-climate-change); question 3 is fairly WG III (mitigation, including technical options). I guess they switched questions 1 and 2 round to avoid making the identification too obvious. The conference steering committee report makes it very clear that they are building on the IPCC TAR foundation.

[Read more…] about Exeter conference: Avoiding Dangerous Climate Change

Filed Under: Climate modelling, Climate Science, Greenhouse gases

Peer Review: A Necessary But Not Sufficient Condition II

27 Jan 2005 by group

by Michael Mann and Gavin Schmidt

In a previous post, we discussed a number of examples where the “Peer Review” process has failed, and poor papers have been published in the ostensibly peer-reviewed literature. In this context, we revisit our previous discussions of the flawed work of McIntyre and McKitrick (henceforth “MM”). MM published a paper, in the controversial journal Energy and Environment, claiming to “correct” the proxy-based reconstruction of Northern Hemisphere temperatures published by Mann et al (1998–henceforth “MBH98”). Following the all-too-familiar pattern, this deeply flawed paper was heavily promoted by special interests as somehow challenging the scientific consensus that humans are altering the climate (an excellent account is provided by science journalist Dan Vergano of USA Today here). As detailed already on the pages of RealClimate, this so-called ‘correction’ was nothing more than a botched application of the MBH98 procedure, where the authors (MM) removed 80% of the proxy data actually used by MBH98 during the 15th century period (failing in the process to produce a reconstruction that passes standard “verification” procedures–an error that is oddly similar to that noted by Benestad (2004) with regard to another recent McKitrick paper). Indeed, the bizarre resulting claim by MM of anomalous 15th century warmth (which falls within the heart of the “Little Ice Age”) is at odds with not only the MBH98 reconstruction, but, in fact the roughly dozen other estimates now published that agree with MBH98 within estimated uncertainties.

[Read more…] about Peer Review: A Necessary But Not Sufficient Condition II

Filed Under: Climate Science, Paleoclimate

Anomalous Recent Warmth in Europe

24 Jan 2005 by group

Translations: (Français)

Guest Contribution by Juerg Luterbacher, University of Bern, Switzerland

While the anomalous nature of recent trends in global average temperature is often highlighted in discussions of climate change, changes at regional scales have potentially greater societal significance. Of particular interest, for example, is the possible relationship between climate change and the incidence of summer heat waves [Meehl, G.A. and C. Tebaldi, Science, 305, 994-997 , 2004] such as those observed in Europe during summer 2003 [see Schaer et al, Nature 427, 332-336 2004; Stott et al, Nature, 432, 610-614­, 2004]. Preliminary analyses of the annual mean surface air temperatures for Europe for 2004 show it be among the few warmest (though not as warm as 1989, 1990, and 1999-2003) since widespread instrumental records have been kept (roughly the past 150 years). 2004 exceeded the reference period (1961-1990) mean temperature by more than 0.8°C. The largest deviations were found over Northern and Eastern Europe. Every single month of 2004 contributed to the overall warmth; February-April, August, October and December were all more than 1°C warmer than the 1961-1990 period. Annual mean European surface air temperatures have increased by around 0.85°C over the last 100 years. The upward trend has accelerated in recent decades, with about 1.2°C of warming taking place over the past 30 years (1975 to 2004). Indeed, the last thirty years likely represent the warmest multidecadal period for Europe in at least the past half millennium [ Luterbacher, J., Dietrich, D., Xoplaki, E., Grosjean, M. and H. Wanner, Science, 303, 1499-1503, 2004], while the last decade (1995-2004) is likely the warmest decade, and summer 2003 the warmest summer. These conclusions are similar to those reached for the entire Northern Hemisphere on the whole.

Filed Under: Climate Science, Instrumental Record, Paleoclimate

Peer Review: A Necessary But Not Sufficient Condition

20 Jan 2005 by group

Translations: (Français)

by Michael Mann and Gavin Schmidt

On this site we emphasize conclusions that are supported by “peer-reviewed” climate research. That is, research that has been published by one or more scientists in a scholarly scientific journal after review by one or more experts in the scientists’ same field (‘peers’) for accuracy and validity. What is so important about “Peer Review”? As Chris Mooney has lucidly put it:

[Peer Review] is an undisputed cornerstone of modern science. Central to the competitive clash of ideas that moves knowledge forward, peer review enjoys so much renown in the scientific community that studies lacking its imprimatur meet with automatic skepticism. Academic reputations hinge on an ability to get work through peer review and into leading journals; university presses employ peer review to decide which books they’re willing to publish; and federal agencies like the National Institutes of Health use peer review to weigh the merits of applications for federal research grants.

[Read more…] about Peer Review: A Necessary But Not Sufficient Condition

Filed Under: Climate Science, Instrumental Record, Paleoclimate, Sun-earth connections

Global Dimming II

19 Jan 2005 by group

Translations: (Français)

Guest commentary on BBC documentary on “Global Dimming” aired on January 13th 2005 by Beate Liepert, LDEO, Columbia University

I haven’t yet seen the documentary. I have only read the transcript and hence was spared the pictures of the potential apocalypse and the invocation of biblical-scale famines. However, as one of the lead scientists on the topic [and who was interviewed by the BBC for the Horizon documentary (transcript, previous post)], I feel I should explain a few things about it without using religious analogies and stoking unnecessary fear.

First though, this is a nice example of the power of words: Gerry Stanhill coined the observed reduction in solar energy reaching the ground “global dimming”. He called it “global” dimming because the technical term for the radiative energy is called “global solar radiation” and it contrasts nicely with the more common “global warming”.

[Read more…] about Global Dimming II

Filed Under: Aerosols, Climate modelling, Climate Science

The global cooling myth

14 Jan 2005 by group

Translations: (Français)

Every now and again, the myth that “we shouldn’t believe global warming predictions now, because in the 1970’s they were predicting an ice age and/or cooling” surfaces. Recently, George Will mentioned it in his column (see Will-full ignorance) and the egregious Crichton manages to say “in the 1970’s all the climate scientists believed an ice age was coming” (see Michael Crichton’s State of Confusion ). You can find it in various other places too [here, mildly here, etc]. But its not an argument used by respectable and knowledgeable skeptics, because it crumbles under analysis. That doesn’t stop it repeatedly cropping up in newsgroups though.

[Read more…] about The global cooling myth

Filed Under: Climate Science, FAQ, Greenhouse gases, Instrumental Record, Paleoclimate

Senator Inhofe on Climate Change

10 Jan 2005 by group

by Michael Mann, Stefan Rahmstorf, Gavin Schmidt, Eric Steig, and William Connolley

Senator James Inhofe (R) of Oklahoma recently provided us with an update of his views on the issue of climate change in a speech given on the opening senate session, January 4, 2005. His speech opened with the statement:

As I said on the Senate floor on July 28, 2003, “much of the debate over global warming is predicated on fear, rather than science.” I called the threat of catastrophic global warming the “greatest hoax ever perpetrated on the American people,” a statement that, to put it mildly, was not viewed kindly by environmental extremists and their elitist organizations.

Cutting through much of his polemic, Inhofe’s speech contains three lines of scientific argument which, according to him, provide “compelling new scientific evidence” that anthropogenic global warming is not threatening. We here submit his statements to scrutiny.
[Read more…] about Senator Inhofe on Climate Change

Filed Under: Arctic and Antarctic, Climate modelling, Climate Science, Greenhouse gases, Paleoclimate

Just what is this Consensus anyway?

22 Dec 2004 by group

Translations: (Français)

We’ve used the term “consensus” here a bit recently (see our earlier post on the subject), without ever really defining what we mean by it. In normal practice, there is no great need to define it – no science depends on it. But it’s useful to record the core that most scientists agree on, for public presentation. The consensus that exists is that of the IPCC reports, in particular the working group I report (there are three WG’s. By “IPCC”, people tend to mean WG I). Fortunately that report is available online for all to read at http://www.grida.no/climate/ipcc_tar/wg1/. It’s a good idea to realise that though the IPCC report contains the consensus, it didn’t form it. The IPCC process was supposed to be – and is – a summary of the science (as available at the time). Because they did their job well, it really is a good review/summary/synthesis.

[Read more…] about Just what is this Consensus anyway?

Filed Under: Climate Science, FAQ

Aerosol

21 Dec 2004 by group

Translations: (Français)

A collection of airborne solid or liquid particles, with a typical size between 0.01 and 10 µm and residing in the atmosphere for at least several hours. Aerosols may be of either natural or anthropogenic origin. Aerosols may influence climate in two ways: directly through scattering and absorbing radiation, and indirectly through acting as condensation nuclei for cloud formation or modifying the optical properties and lifetime of clouds (from the always useful IPCC glossary).

See-also: wiki:Aerosol.

Filed Under: Glossary

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