Hello pmaust, I don't have much time but let me respond briefly to your comments and links
To say water vapor is not a dominant greenhouse gas is incorrect (the name of one of Infinite's links). In fact, if you remove all the water vapor you can easily simulate a snowball earth, and taking it away results in a reduction of around 60% of the longwave absorbed. (See table 3
Earth’s Annual Global Mean Energy Budget)
However, "greenhouse gas," or "greenhouse effect," and "global warming" are two different things. "Feedback not a forcing" is a good simple answer, and is indicative of water vapor's strong impact on the temperature, but it does not provide any answer for the "change in" temperature observed over the last century. Global warming is about the change. And water vapor follows along with any temperature change, amplifying that change in the way it was going. Just to advertise my blog again, see my post at
"Basic Radiative models/Earth’s climate system analysis Pt. 2"
There, I talk a bit about the radiative physics of the greenhouse effect, and the relationship of water vapor to temperature, and its role in climate change. If you have any comments, criticisms, questions, let me know.
Regarding the first icecap reference by Joseph D’Aleo, this link actually does not discuss the global mean temperature, but the United States mean temperature (tricky, eh). However, the third graph in that link refutes the basic premise of the post (the article is clearly not intended for those familair with radiative physics, but people who just like to see lines going up together). Note the Y axis for the TSI. At most, I would say you can get 2 W/m^2 of a change in TSI (total solar irradiance) from the pre-industrial time. To convert this into a radiative forcing on Earth, you need to divide by 4 (for the geometry of the Earth), and multiply by 0.69 to account for the albedo of the Earth. Ideally, you'd still need to account for efficacy, and the UV radiation absorbed at the stratosphere which would further lower the number, but this is typically not done in the primary literature: So you end up with around .35 W/m^2 of radiative forcing, compared to the 1.66 W/m^2 from just CO2. This is past the high end in the IPCC document, because IPCC is relative to 1750, and the ΔTSI of 2 W/m^2 is probably high. Here is the
IPCC forcings chart
Regarding Spencer's post, there are much better sources out there. The first points on water vapor are addressed in my blog, and if you want more reliable sources than me, I can reference you to several from the peer review that refute the "Water vapor overwhelms CO2" nonsense. There are a lot of other claims in his post- some true, some false. The literature does not support his point on the medieval warm period, and that really has nothing to do with what is causing it today. The post itself seems to come down to his view on feedbacks. Spencer ( I think) notes somewhere in there that the temperature change is about 1 degree with just 2x CO2 increase (1.2 C actually). That part is basic physics. What is more uncertain is feedbacks, notably cloud responses. There are many cloud feedbacks, on amount, height, optical thickness, etc., and different for different cloud types and at different latitudes. Overall, today's models produce cloud feedbacks ranging from approximately neutral to strongly positive. There could be an overall negative cloud feedback but it couldn't be very strong, because we have data that show that overall low clouds, which control the albedo more than any other kind, get thinner when it gets warmer.
There are several academic sources which go over this,
Pubs.GISS: Abstract of Bony et al. 2006
http://www.gfdl.noaa.gov/reference/b...06/bjs0601.pdf
and the free,online book from the NAtional Academies
Understanding Climate Change Feedbacks
Ch. 8 in the AR4 is also a good place to start.
There is no question that cloud feedbacks are uncertain and that modeling them is hard -- I don't think that anyone has ever seriously claimed otherwise. Another thing is that to argue for the 3 C rise per 2x CO2 by the IPCC, you do need to argue for a positive cloud feedback (the range is 2-4.5 C, and real world observations are putting confidence in this rather than wishful thinking). Putting faith in Spencer's rather contrarian view that we will be saved by a hypothetical strong negative feedback (also pushed by Lindzen) is not much better.
chris
And sorry for the link format, still a few more posts to go
(Moderator note: per suggestion, made url references into links)