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Climate modelling

Busy Week for Water Vapor

21 Nov 2005 by raypierre

It’s been a busy week for water vapor, and I have two recent papers to discuss. The first is the paper "Anthropogenic greenhouse forcing and strong water vapor feedback increase temperature in Europe" by Rolf Philipona et al. (GRL, 2005, subscription required for full text), which has attracted a certain amount of media attention. The overall goal of the paper is to understand, from a physical standpoint, why European temperatures have been increasing three times faster than the Northern Hemisphere average. It focuses on the changes between 1995 and 2002, over which time good surface radiation budget observations are available. The paper reports some results on the role of large scale circulation changes (which they conclude are minor) but I’ll concentrate on the results relating to water vapor.

[Read more…] about Busy Week for Water Vapor

Filed Under: Climate modelling, Climate Science, Greenhouse gases

Chaos and Climate

4 Nov 2005 by group

By James Annan and William Connolley

In this post, we will try to explain a little about chaos theory, and its relevance to our attempts to understand and forecast the climate system. The chaotic nature of atmospheric solutions of the Navier-Stokes equations for fluid flow has great impact on weather forecasting (which we discuss first), but the evidence suggests that it has much less importance for climate prediction.

[Read more…] about Chaos and Climate

Filed Under: Climate modelling, Climate Science

Modeller vs. modeller

20 Oct 2005 by Gavin

We recently got a request from Tom Cole, a water quality researcher, to explain some of the issues in climate modelling seen from his perspective as a fellow numerical modeller. His (slightly paraphrased) questions are the basis for this post, and hopefully the answers may provide some enlightment for modellers and non-modellers alike! [Read more…] about Modeller vs. modeller

Filed Under: Climate modelling, Climate Science

Global warming on Mars? Réchauffement global sur Mars ?

5 Oct 2005 by group

Guest contribution by Steinn Sigurdsson.

Recently, there have been some suggestions that “global warming” has been observed on Mars (e.g. here). These are based on observations of regional change around the South Polar Cap, but seem to have been extended into a “global” change, and used by some to infer an external common mechanism for global warming on Earth and Mars (e.g. here and here). But this is incorrect reasoning and based on faulty understanding of the data.
Article invité par Steinn Sigurdsson. (traduit par Claire Rollion-Bard)

Récemment, il y a eu des suggestions qu’un “réchauffement global” a été observé sur Mars (par exemple, ici). Ceci est basé sur des observations d’un changement régional autour de la calotte polaire sud, mais semble avoir été étendu à un changement “global” et utilisé par certains pour en déduire un mécanisme commun externe pour le réchauffement global sur la Terre et sur Mars. (par exemple, ici et ici). Mais c’est un raisonnement incorrect et basé sur une mauvaise compréhension des données.
[Read more…] about Global warming on Mars? Réchauffement global sur Mars ?

Filed Under: Climate modelling, Climate Science, FAQ, Sun-earth connections

Inhofe and Crichton: Together at Last!

28 Sep 2005 by group

Gavin Schmidt and Michael Mann

Today we witnessed a rather curious event in the US Senate. Possibly for the first time ever, a chair of a Senate committee, one Senator James Inhofe (R-Oklahoma), invited a science fiction writer to advise the committee (Environment and Public Works), on science facts–in this case, the facts behind climate change. The author in question? None other than our old friend, Michael Crichton whom we’ve had reason to mention before (see here and here). The committee’s ranking member, Senator James Jeffords (I) of Vermont, was clearly not impressed. Joining Crichton on climate change issues was William Gray of hurricane forecasting fame, Richard Benedick (a negotiator on the Montreal Protocol on ozone-depleting chemicals), and David Sandalow (Brookings Institution). As might be expected, we paid a fair bit of attention to the scientific (and not-so-scientific) points made. [Read more…] about Inhofe and Crichton: Together at Last!

Filed Under: Climate modelling, Climate Science

What is a first-order climate forcing?

22 Sep 2005 by Gavin

Roger Pielke Sr. (Colorado State) has a blog (Climate Science) that gives his personal perspective on climate change issues. In it, he has made clear that he feels that apart from greenhouse gases, other climate forcings (the changes that affect the energy balance of the planet) are being neglected in the scientific discussion. Specifically, he feels that many of these other forcings have sufficient ‘first-order’ effects to prevent a clear attribution of recent climate change to greenhouse gases.

In general, I heartily agree – other forcings are important, even essential, for understanding observed climate variability and, as a community, we are only just starting to get to grips with some of the more complicated effects. Obviously, though, not all forcings are of the same magnitude (either globally or regionally) and so it is useful to separate the ‘first-order’ forcings from those that are relatively minor. But what exactly is ‘first-order’ and what is not? [Read more…] about What is a first-order climate forcing?

Filed Under: Aerosols, Climate modelling, Climate Science, Greenhouse gases

Hurricanes and Global Warming – Is There a Connection? Huracanes y calentamiento global ¿Hay conexión?Ouragans et réchauffement global – existe t’il un lien ?

2 Sep 2005 by group

by Stefan Rahmstorf, Michael Mann, Rasmus Benestad, Gavin Schmidt, and William Connolley

On Monday August 29, Hurricane Katrina ravaged New Orleans, Louisiana and Missisippi, leaving a trail of destruction in her wake. It will be some time until the full toll of this hurricane can be assessed, but the devastating human and environmental impacts are already obvious.

Katrina was the most feared of all meteorological events, a major hurricane making landfall in a highly-populated low-lying region. In the wake of this devastation, many have questioned whether global warming may have contributed to this disaster. Could New Orleans be the first major U.S. city ravaged by human-caused climate change?

[lang_fr]
by Stefan Rahmstorf, Michael Mann, Rasmus Benestad, Gavin Schmidt, and William Connolley (traduit par Claire Rollion Bard)
Le lundi 29 août, l’ouragan Katrina a ravagé la Nouvelle-Orléans, la Louisiane et le Mississipi, laissant une traînée de destruction dans son sillage. Il va se passer du temps avant que le bilan total de cet ouragan soit estimé, mais les impacts environnementaux et humains sont déjà apparents.
Katrina était le plus craint des évènements météorologiques, un ouragan majeur laissant un terrain vide dans une région très peuplée de faible élévation. Dans le sillage de sa dévastation, beaucoup se sont demandés si le réchauffement global pouvait avoir contribué à ce désastre. La Nouvelle-Orléans pourrait-elle être la première ville majeure des Etats-Unis à être ravagée par le changement climatique causé par les humains ?
(suite…)

[\lang_fr]

[Read more…] about Hurricanes and Global Warming – Is There a Connection? Huracanes y calentamiento global ¿Hay conexión?Ouragans et réchauffement global – existe t’il un lien ?

Filed Under: Climate modelling, Climate Science, El Nino, FAQ, Hurricanes, Instrumental Record, Oceans

Et Tu LT?

11 Aug 2005 by Gavin

In previous posts we have stressed that discrepancies between models and observations force scientists to re-examine the foundations of both the modelling and the interpretation of the data. So it has been for the apparent discrepancies between the Microwave Sounding Unit (MSU) lower tropospheric temperature records (MSU 2LT), radiosonde records and the climate models that try to simulate the climate of the last few decades. Three papers this week in Science Express, Mears et al, Santer et al (on which I’m a co-author) and Sherwood et al show that the discrepancy has been mostly resolved – in favour of the models.

[Read more…] about Et Tu LT?

Filed Under: Climate modelling, Climate Science, Instrumental Record

The lure of solar forcing

15 Jul 2005 by Gavin

It’s obvious.

The sun provides 99.998% of the energy to the Earth’s climate (the rest coming from geothermal heat sources). The circulation patterns of the tropical Hadley Cell, the mid latitude storm tracks the polar high and the resulting climate zones are all driven by the gradients of solar heating as a function of latitude. So of course any significant change to solar output is bound to affect the climate, it stands to reason! Since we can see that there are changes in solar activity, it’s therefore just a question of finding the link. Researchers for over a century have therefore taken any climate records they can find and searched for correlations to the sunspots, the solar-cycle length, geomagnetic indices, cosmogenic isotopes or smoothed versions thereof (and there are many ways to do the smoothing, and you don’t even need to confine yourself to one single method per record). At the same time, estimates of solar output in the past are extremely uncertain, and so there is a great deal of scope in blaming any unexplained phenomena on solar changes without fear of contradiction.

[Read more…] about The lure of solar forcing

Filed Under: Climate modelling, Climate Science, Sun-earth connections

Planetary energy imbalance?

3 May 2005 by Gavin


The recent paper in Science Express by Hansen et al (on which I am a co-author) has garnered quite a lot of press attention and has been described as the ‘smoking gun’ for anthropogenic climate change. We have discussed many of the relevant issues here before, but it may be useful to go over the arguments again here.

The key points of the paper are that: i) model simulations with 20th century forcings are able to match the surface air temperature record, ii) they also match the measured changes of ocean heat content over the last decade, iii) the implied planetary imbalance (the amount of excess energy the Earth is currently absorbing) which is roughly equal to the ocean heat uptake, is significant and growing, and iv) this implies both that there is significant heating “in the pipeline”, and that there is an important lag in the climate’s full response to changes in the forcing.

[Read more…] about Planetary energy imbalance?

Filed Under: Climate modelling, Climate Science, Greenhouse gases, Oceans

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