Showing posts with label RealClimate. Show all posts
Showing posts with label RealClimate. Show all posts

Friday, May 13, 2011

Peer criticism -- REVISED version of Rancourt radiation physics paper

[Prof. Ray Pierrehumbert]
  1. Rancourt writes original version of article, HERE.
  2. Asks for and receives peer criticism, HERE.
  3. Rancourt writes significantly revised version of article, HERE.
  4. Asks for and receives further peer criticism about revised version, PRESENT POST.
  5. It appears that Rancourt's revised paper is correct: The predicted effect of CO2 is two orders of magnitude smaller than the effects of other parameters.
  6. Final June 2011 (Third) version is significantly augmented, LINK-HERE.

Following the posting of THIS significantly revised version of Denis Rancourt's paper about Earth's radiation balance, Rancourt asked the climate scientists at RealClimate for follow-up criticism -- resulting in this email exchange:

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From: Denis Rancourt
Date: Thu, May 12, 2011 at 3:57 PM
Subject: Re: climate
To: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, rtp1@geosci.uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Revised version posted:
http://climateguy.blogspot.com/2011/05/radiation-physics-constraints-on-global_12.html

Please provide any feedback.

Denis Rancourt

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From: Eric Steig
Date: Thu, May 12, 2011 at 4:28 PM
Subject: Re: climate
To: Denis Rancourt
Cc: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, rtp1@geosci.uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Denis,

I applaud your efforts to take Ray's criticisms into account, but your post is still full of errors. I really don't have the time to get into all of them, but case in point is where you write that

"The longwave atmospheric absorption in the CO2 absorption band is saturated in Earth conditions and this is important because it is the physical reality ..."

This is simply wrong. See here: for example an explanation of why.

http://www.realclimate.org/index.php/archives/2007/06/a-saturated-gassy-argument/

Eric Steig

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From: Raymond P.
Date: Thu, May 12, 2011 at 6:22 PM
Subject: Re: climate
To: Denis Rancourt
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Yes, Denis, Eric is right about that. I did say that your failure to understand Kirchoff's law was only ONE of the problems with your post. I collaborated on writing the post Eric refers to, and I also wrote the accompanying post on "What Angstrom didn't know"

I appreciate your efforts to learn this material, but writing nonsense and having us correct it bit by bit is very inefficient of everybody's time. I suggest that before you make such sweeping pronouncements about the subject, you take the time to educate yourself on the basics. David Archer's book, "Understanding the Forecast" is a good place to start, and you can follow that with my book, Principles of Planetary Climate." For that matter, if you had read my Physics Today article, which I pointed out to you in connection with the G&T nonsense, you would have already known about the saturation fallacy.

--Ray

------------------------------------------

From: Denis Rancourt
Date: 2011/5/12
Subject: Re: climate
To: "Raymond P."
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Hi Ray and Eric,

Actually, Ray, the first version did not use the saturation approach so this could not have been an error in the first version.

The physical model I now use is a single-layer atmosphere that is longwave opaque withing a certain width on the main CO2 band and that does not emit at other wavelengths. It either lets ground longwave through or it blocks it within this "saturation band". The width of the assumed saturation opaqueness band increases with CO2 content by assuming a binary cutoff of transmission/opaqueness at a characteristic value of cross section giving opaqueness and a Gaussian cross section profile.

While these are simplifying assumptions they do not violate any physical law or principle. One can argue that the longwave absorption of the real atmosphere can be approximately parametrized in this way.

The model clearly shows how a saturating atmosphere would work (in the limit of black/white saturation circumstances) regarding surface temperature, without using a full thick infrared radiative transfer theory calculation. The model treats only the atmosphere's role in blocking or letting through ground thermal emission. It says that role for the CO2 15 um band works this way.

It seems to me that the (one-layer) atmosphere's own thermal emission is not relevant because half goes up and out while half goes down and back to be fully absorbed (e ~ 1). In the limit of all-thermalization of absorbed longwave, this only means that ~half that is resonantly absorbed at saturation actually gets out. This is easily handled by reducing the cross section by a factor of ~two. This factor of two would appear in the "ln(σm/σe)" term of my equations 8 and 9 and therefore would have no significant effect.

Therefore it appears that your negation relies mostly on the differences that there would be between a one-layer radiating and absorbing atmosphere and a thick (multi-layer) atmosphere. It seems to me that this would only lead to yet another small re-normalization of my characteristic model parameters. But I will examine this.

Do you have a simple code that simulates the radiation transfer in a multi-layer model atmosphere?

Thank you for your help.

-denis

--------------------------------------------------

From: Denis Rancourt
Date: 2011/5/12
Subject: Re: climate
To: "Raymond P."
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Also, is it possible that you did not read my revised article beyond the word "saturation"?

I actually apply what you describe here:
http://www.realclimate.org/index.php/archives/2007/06/a-saturated-gassy-argument-part-ii/comment-page-13/#comments

The only difference is that I make the estimation quantitative by using a Gaussian shape cross section and a sharp cut-off.

The warming on increasing CO2 in my model directly comes from the extra absorption in the wings of the band...

-denis

-------------------------------------------------------

From: Raymond P.
Date: Thu, May 12, 2011 at 9:00 PM
Subject: Re: climate
To: Denis Rancourt
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Denis, you are making a small amount of progress. The single layer version catches up with Arrhenius, and (when used with modern spectroscopy) has the exact same problems that Arrhenius had, as only became clear later when things got sorted out in the 60's by Manabe. There is a full discussion of this in The Warming Papers.

I still recommend you would do better to educate yourself on the basics, and show a bit of humility about those things of which you are ignorant, before you make sweeping pronouncements.

--Ray

---------------------------------------------------------

From: Raymond P.
Date: Thu, May 12, 2011 at 10:05 PM
Subject: Re: climate
To: Denis Rancourt
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Dear Denis,

This conversation started out well, but now it's degenerating. I was pleased that you were able to learn something about Kirchoff's Law, and were willing to update your essay to correct that blunder. Every little bit that eliminates propagation of nonsense, and gets some truth out into the arena, is a step forward. But you still clearly have a lot to learn, and I'm suspicious because so far as I can tell, you seem to have made up your mind before you even have gotten pinkie deep into learning the subject matter you'd need to pass judgment.

So, what's especially on my mind (and I would love to be proved wrong) is that back in 2007 you declared that the entire man made global warming movement is nothing more than "a corrupt social phenomenon." That statement has been featured prominently by Marc Morano, which is indeed where I first came across your name. This quote has been picked up widely by inactivists everywhere, and is particularly choice to that community because it comes from a self-professed leftist.

So were you quoted fairly? If not, have you ever taken steps to rectify the way your name is being used? If you were indeed quoted correctly, to you still stand by this statement? Have you ever retracted it in the face of things you have learned since? I am much disturbed by the fact that you would make such a statement years before you had progressed to the point where you even understood Kirchoff's Law (that point being evidently the day before yesterday, or thereabouts). How can you justify having made such a pronouncement at a time when you had such a thoroughly inadequate understanding of the subject? And, the fact is, you still have a thoroughly inadequate understanding of the subject.

I would like to think that we have some common ground, but I need an explanation as to how in the world you came to the opinion you expressed without having an inkling of the physical basis of the subject.

--Ray

------------------------------------------------

From: Denis Rancourt
Date: Thu, May 12, 2011 at 10:44 PM
Subject: Re: climate
To: "Raymond P."
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Hi Ray,

It's good that you accepted to engage on the science despite my political statements.

I think it is possible to examine and evaluate the science separately from our evaluation of the political and social forces that drive the science establishment.

I also think that one can evaluate the latter without being a specialist in the former. Otherwise, we will need to eliminate the field of social history of science and technology.

In addition, my understanding of the science, having corrected my Kirchoff's Law error and having implemented a reasonable model of longwave absorption by CO2, suggests that my "sweeping statements" about the science are worthy of attention.

In particular, given the simplicity of my model, you would need to provide a quantitative estimate showing how my single-layer model with the correct absorption cross section and relevant characteristic parameters can be off in terms of estimated relative sensitivities compared to a multi-layer model.

Since my model uses the most straightforward and simplest assumptions and the actual known characteristic parameters, you need to show where it is wrong, beyond waving a broad "read my book - multi-layer or die" magic wand.

Is that not fair for a seasoned expert such as yourself?

I have already demonstrated how I respond to being correctly shown to be in error. And I assure you that I am open to changing my views.

Do you have a simple code that simulates the radiation transfer in a multi-layer model atmosphere? (If not, then how do you gauge the importance of using a multi-layer model?)

cheers,
-denis

-----------------------------------------------

From: Denis Rancourt
Date: Fri, May 13, 2011 at 5:44 PM
Subject: Re: climate
To: "Raymond P."
Cc: Gavin Schmidt , mann@psu.edu, ammann@ucar.edu, Rasmus Benestad , Ray Bradley , Stefan Rahmstorf , Stefan Rahmstorf , Eric Steig , Eric Steig , David Archer , garidel@marine.rutgers.edu, Jim Bouldin , William Connolley

Dear Ray,

I have posted our exchange here:
http://climateguy.blogspot.com/2011/05/peer-criticism-revised-version-of.html

(The picture links to your web site.)

I await any next installment in our communication about these simple models that allow an estimation of climate sensitivity to different key parameters.

best,
-denis

-----------------------------------------------

Peer criticism -- Original version of Rancourt radiation physics paper

Following THIS request for peer criticism of THIS original version of a paper about Earth's radiation balance, the following email exchange occurred.

---------------------------------------

From: Michael Mann [mem45]
Date: Tue, May 10, 2011 at 4:10 PM
Subject: Re: climate
To: denis rancourt

I will be away from my email through May 14, 2011.

Any email sent before then may remain unread and be discarded. If your message is important, you will need to resend after that date.

-------------------------------

From: Raymond P.
Date: Tue, May 10, 2011 at 4:24 PM
Subject: climate
To: Denis Rancourt
Cc: allrc

Dear Mr. Rancourt,

Your discussion of energy balance starts off soundly, but then you get mired in a nest of mistakes, the most critical of which is your misunderstanding of Kirchoff's Law. Kirchoff's law only requires that emissivity and absorptivity be equal at the same wavelength. Since Earth's incoming radiation is shortwave, but outgoing is longwave (infrared), there is no contradiction between a surface emissivity near unity and an albedo of around 0.3 . Your calculation erroneously attributes the effect of atmospheric infrared opacity to surface emissivity.

By the way, climate models do not assume surface infrared emissivity to be unity. The deviations from unity are not a major effect in the surface budget, but the emissivity of common Earth materials can be easily measured, and in full GCM's the emissivity is taken into account in the lower boundary condition for radiation models.

Thank you for your interest in this subject.

--Ray Pierrehumbert

--------------------------------

From: Denis Rancourt
Date: Tue, May 10, 2011 at 5:05 PM
Subject: Re: climate
To: "Raymond P."
Cc: allrc , gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Dear Mr. Pierrehumbert,

Thank you for your critique. I will post it. You are correct that Kirchoff's Law strictly applies for a given wavelength and that I took it to apply at all wavelengths for a given material. (I took albedo and emissivity to be wavelength-independent. This could indeed be rather off, depending on the material.)

Could you point me to a paper where shortwave albedo and longwave emissivity were measured in a common Earth material?

Do you believe that a correct longwave emissivity for Earth is 1 and that therefore the atmosphereless Earth would be at -19C? This is stated on the RealClimate web site.

Also, it would be useful if you could state what other errors you have found in the article, since you have already ascertained these errors.

Sincerely,
Denis Rancourt

---------------------------------

From: Raymond P.
Date: Wed, May 11, 2011 at 12:11 AM
Subject: Re: climate
To: Denis Rancourt
Cc: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Emission-weighted emissivity is one of the easiest quantities to measure. It is even routinely used in engineering studies. Detaied spectrally resolved emissivity measurements are routinely reported in Icarus and JSQRT, since they are crucial to the use of infrared spectroscopy in estimating mineral composition of planetary surfaces. The literature is far too vast to summarize, but an example of some typical emissivities at various temperatures for common building and terrestrial materials is listed, for exampe, at:

http://www.coleparmer.com/techinfo/techinfo.asp?htmlfile=Emissivity.htm&ID=254#anchor4

Also emissivity can be computed in a straightforward way from measured absorption coefficients of condensed substances. Detailed data for water, water ice and CO2 ice is given in Chapter 4 and 5 of my book, Principles of Planetary Climate. Data sets and references are found on the book web site. (go to geosci.uchicago.edu/~rtp1 and follow links to ClimateBook).

The emissivity of ice and water, which makes up most of the surface of the Earth, is very accurately known. The emissivity of land varies more, especially in response to vegetation cover, but it is known well enough for the purposes of determining energy balance; there can be problems with microwave emissivity of land surfaces which complicate doing microwave retrievals over land in some circumstances.

I do not actually agree with the statement that the Earth's temperature would be -19C if you removed the atmosphere. This is a true statement of what you would get if you replaced the atmosphere with an IR-transparent atmosphere (e.g. N2), which could still transport heat, and if moreover you could prevent the ocean from freezing over. In reality, if you did that, the oceans would freeze, and the mean temperature would be much colder than -19C (see my AREPS Neoproterozoic review article for numbers). But if the Earth had no oceans and you took away the atmosphere, first of all, you would also take away the clouds (which changes the albedo) and second of all you would take away heat transport. In that case, the temperature distribution would be rather like the Moon -- 100C at the subsolar point, maybe -100C on the night side. (Slightly warmer than the Moon on the night side, because the Earth is more rapidly rotating, so there's less time for the surface to cool down).

But there is absolutely zero question that removing CO2 from the Earth's atmosphere would make it much colder than -19C, and probably cause the Earth to turn into a snowball. The radiation physics of this is unassailable, and based on more than a century of work by some of the best physicists around, backed up by thousands of laboratory and satellite measurements. You are really barking up the wrong tree.

--Ray Pierrehumbert

-----------------------------------

From: Denis Rancourt
Date: Wed, May 11, 2011 at 8:40 AM
Subject: Re: climate
To: "Raymond P."
Cc: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Thank you for your detailed response.

From now on, whenever I describe the simple radiation balance equations I will stress that the albedo is for shortwave whereas the emissivity is for longwave (and that Kirchoff's Law therefore is not relevant). That arbitrary step of setting emissivity equal to 1 in textbook descriptions (without explaining that water and vegetation emissivities are close to 1) always bothered me, since I was 18 in first year.

I will make a revised article and I will also correct others who may make the same error about Kirchoff's Law.

Thanks.

Denis Rancourt

-------------------------------------

From: Raymond P.
Date: Wed, May 11, 2011 at 8:55 AM
Subject: Re: climate
To: Denis Rancourt

No problem. Radiation balance and planetary temperature is a really fascinating subject, and I'm always happy when people take in interest in it. You might be interested in some of the classic papers Dave Archer and I compiled (with interpretive essays) in our book, "The Warming Papers" -- particularly the things Arrhenius did or didn't get right, the false steps along the way (e.g. Plass getting mired in a surface budget fallacy) and the way Manabe finally got everything right in the 60's. It's pubished by Wiley/Blackwell. The pricetag unfortunately got rather high, but that was out of our control, since most of the cost of the book was in copyright fees payed to copyright holders for permission to reprint.

--Ray

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...
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From: Denis Rancourt
Date: Thu, May 12, 2011 at 3:57 PM
Subject: Re: climate
To: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, rtp1@geosci.uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wconnolley

Revised version posted:
http://climateguy.blogspot.com/2011/05/radiation-physics-constraints-on-global_12.html

Please provide any feedback.

Denis Rancourt

----------------------------------------

Note: The June 2011 (third and final) version of Rancourt's paper, corrected and largely augmented is LINK-HERE.

Tuesday, May 10, 2011

Request to RealClimate scientists


From: Denis Rancourt <>
Date: Tue, May 10, 2011 at 4:10 PM
Subject: climate
To: gschmidt@giss.nasa.gov, mann@psu.edu, ammann@ucar.edu, rasmus.benestad@met.no, rbradley@geo.umass.edu, rahmstorf@ozean-klima.de, rahmstorf@pik-potsdam.de, steig@u.washington.edu, d-archer@uchicago.edu, rtp1@geosci.uchicago.edu, garidel@marine.rutgers.edu, jrbouldin@ucdavis.edu, wmconnolley@gmail.com


Dear Gavin Schmidt, Michael Mann, Caspar Ammann, Rasmus Benestad, Ray Bradley, Stefan Rahmstorf, Eric Steig, David Archer, Ray Pierrehumbert, Thibault de Garidel, Jim Bouldin, and William Michael Connolley,

Dear contributors to Real Climate,

Dear colleagues,

Re: A new article for your review

Please consider this new article:
"Radiation physics constraints on global warming"
http://activistteacher.blogspot.com/2011/05/radiation-physics-constraints-on-global.html

I believe this article contains proof of incorrect/unjustified assumptions and corresponding results published on the Real Climate web site.

I would welcome your reviews of my article for posting.

I will feature all your comments and criticisms on the same blog.

Sincerely,
Denis Rancourt, B.Sc., M.Sc., Ph.D. (Physics)
Former professor and environmental researcher, University of Ottawa, Canada
http://rancourt.academicfreedom.ca/blogs-etc/scientific-work.html