In this article in the series we will look an interesting paper: An analysis of the dependence of clear-sky top-of-atmosphere outgoing longwave radiation on atmospheric temperature and water vapor, by Dessler, Yang, Lee, Solbrig, Zhang and Minschwaner, JGR (2008). This paper can be downloaded for free. I used some results of this paper in Theory and Experiment [...]
Archive for the ‘Feedback’ Category
Clouds and Water Vapor – Part Four
Posted in Atmospheric Physics, Feedback on March 17, 2011 | 47 Comments »
Clouds and Water Vapor – Part Three
Posted in Atmospheric Physics, Climate Models, Feedback on September 18, 2010 | 39 Comments »
In Part One we had a look at Ramanathan’s work (actually Raval and Ramanathan) attempting to measure the changes in outgoing longwave radiation vs surface temperature. In Part Two (Part Zero perhaps) we looked at some basics on water vapor as well as some measurements. The subject of the non-linear effects of water vapor was [...]
Clouds and Water Vapor – Part One – Responses
Posted in Atmospheric Physics, Feedback on August 29, 2010 | 104 Comments »
After posting Part Two on water vapor, some people were unhappy that questions from Part One were not addressed. I have re-read through the many comments and questions and attempt to answer them here. I ignore the questions unrelated to the feedbacks of water vapor and clouds – like the many questions about the moon, [...]
Clouds and Water Vapor – Part Two
Posted in Atmospheric Physics, Feedback on August 25, 2010 | 26 Comments »
In Part One we covered a lot of ground. In this next part we will take a look at some basics about water vapor. The response of water vapor to a warmer climate is at the heart of concerns about the effect of increasing the inappropriately-named “greenhouse” gases like CO2 and methane. Water vapor is [...]
Clouds and Water Vapor – Part One
Posted in Atmospheric Physics, Feedback on May 30, 2010 | 130 Comments »
In the CO2 series we looked at the effect of CO2 without climate feedbacks. The “answer” to the doubling of CO2 was a “radiative forcing” of 3.7W/m^2 and an increase in surface temperature of about 1°C. What about feedbacks? There are many ways to introduce this problem. We’ll start with the great Ramanathan, who is [...]

