tag:blogger.com,1999:blog-16612221.post4536405575889728641..comments2024-03-19T03:14:04.172-04:00Comments on Rabett Run: Original ClimateballEliRabetthttp://www.blogger.com/profile/07957002964638398767noreply@blogger.comBlogger11125tag:blogger.com,1999:blog-16612221.post-69570864288347717352017-08-05T16:49:13.655-04:002017-08-05T16:49:13.655-04:00OpenID izenmeme said...
"What evidence do you...OpenID izenmeme said...<br />"What evidence do you have to support the idea that ice albedo loss and methane increases (along with many other factors) will not be larger feedbacks as temperatures increase ?"<br /><br />Well, I'm not going to present much evidence in a comment. The ice-albedo feedback will be mostly done after we reach 2xCO2. I don't know about melting methane clathrates, except that most scientists seem to think now they won't occur before 2100, but you may be right about them. <br /><br />Increasingly I am beginning to think we won't get to 2xCO2. That's still a long-ways off, +150 ppm, less than we're at now. I don't really know though.<br /><br />What do you think?David Appellhttps://www.blogger.com/profile/03318269033139447591noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-82541367083303179512017-08-05T11:44:28.905-04:002017-08-05T11:44:28.905-04:00thermal: as I previously told you at Roy Spencer&#...thermal: as I previously told you at Roy Spencer's blog, the terms in your equation don't even have consistent units. So right away it's obviously wrong.David Appellhttps://www.blogger.com/profile/03318269033139447591noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-58583585025713029782017-08-05T01:41:03.260-04:002017-08-05T01:41:03.260-04:00Since we are talking about a thermodynamic system ...Since we are talking about a thermodynamic system it should be described with the first law. Which part is "forcing"? Is it Q or W? It has to be one of them.<br />Why is "forcing" unique for gh-theory? Otherwise we have either a force or we don't. <br />We know "forcing" doesn't add any energy, and the heat flow is constant and limited(TSI), then how can Q increase without adding either work or energy?<br /><br />Try this for effective temperature:<br /><br />TSI-4g²=4T(effective)<br /><br />That is ∆U=Q-W. If you don't have the first law, you have nothing.lifeisthermalhttps://www.blogger.com/profile/18007629221165162210noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-2469083382538603332017-07-30T15:13:55.456-04:002017-07-30T15:13:55.456-04:00It's a weakness of all simple parameterization...It's a weakness of all simple parameterization, but also the strength. As long as there is a single overwhelming driver and the system has not been driven too far from it's equilibrium point 2x CO2 does a decent job.EliRabetthttps://www.blogger.com/profile/07957002964638398767noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-53029356222611991082017-07-30T07:20:56.186-04:002017-07-30T07:20:56.186-04:00David Appell --- Yes, climate sensitivity, as usua...David Appell --- Yes, climate sensitivity, as usually defined, is dubiously useful. For example, in the mid-Pliocene the carbon dioxide concentration was about the same as now while the global temperature was 2--3 °C warmer than now. Of course the climate system is currently far from equilibrium so the warming will come as the climate equilibriates. So what, then, is the climate sensitivity? David B. Bensonhttps://www.blogger.com/profile/15914145623997712113noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-76773544700095748822017-07-29T15:54:57.191-04:002017-07-29T15:54:57.191-04:002.2 cheers for feedback mitigation.
If we knew m...2.2 cheers for feedback mitigation.<br /><br /><br />If we knew more about ocean albedo variability arising from marine biology, I might make it 2.3.THE CLIMATE WARShttps://www.blogger.com/profile/02578106673226403151noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-35127284805314602382017-07-29T03:20:36.177-04:002017-07-29T03:20:36.177-04:00Interesting assertion.
What evidence do you have t...Interesting assertion.<br />What evidence do you have to support the idea that ice albedo loss and methane increases (along with many other factors) will not be larger feedbacks as temperatures increase ?<br />What current feedbacks do you envision reducing as temperatures rise ?Anonymousnoreply@blogger.comtag:blogger.com,1999:blog-16612221.post-84810118352330715592017-07-29T03:03:26.690-04:002017-07-29T03:03:26.690-04:00In other words, the problem with defining climate ...In other words, the problem with defining climate sensitivity as dT(2x CO2_0) is that dT(4x CO2_0) is not 2*dT(2xCO2_0), as one would naively expect. The temperature feedbacks in the first doubling of CO2 are likely larger than the feedbacks in the second doubling. <br /><br />In any case, the respective feedbacks are certainly not equal. It's clear that<br /><br />dT/dF = lambda = lambda(T, CO2)<br /><br />and not equal to a constant.<br /><br />Even worse, lambda is sure path dependent (the path being CO2(time)). David Appellhttps://www.blogger.com/profile/03318269033139447591noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-30906953470518791562017-07-29T02:51:54.069-04:002017-07-29T02:51:54.069-04:00What's wrong with dT/dF, where T = surface tem...What's wrong with dT/dF, where T = surface temperature and F = manmade radiative forcing?<br /><br />dT/dF = lambda = climate sensitivity when CO2 = 2x CO2_0, but there's no reason to expect lambda to be a constant over any range of CO2, whether it's doubled, +50%, +150%, or whatever.<br /><br />In other words, lambda is a function of both CO2 and temperature. So it isn't fundamental. <br />David Appellhttps://www.blogger.com/profile/03318269033139447591noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-995521766014019762017-07-29T02:44:16.633-04:002017-07-29T02:44:16.633-04:00David Appell, not really. All are proportions of ...David Appell, not really. All are proportions of one another. David B. Bensonhttps://www.blogger.com/profile/15914145623997712113noreply@blogger.comtag:blogger.com,1999:blog-16612221.post-39869705803595406762017-07-29T00:47:05.282-04:002017-07-29T00:47:05.282-04:00Are there other useful choices?Are there other useful choices?David Appellhttps://www.blogger.com/profile/03318269033139447591noreply@blogger.com