Why Does a CO2 Increase Cool the Stratosphere?

Thursday, 18 December 2014: 3:10 PM
Sergio Sejas, Florida State University, Tallahassee, FL, United States
The cooling of the stratosphere is a robust feature of climate simulations forced by an increase in CO2. This feature is primarily a consequence of the CO2 forcing alone (no feedbacks), which causes longwave (LW) radiative cooling in the stratosphere. In this study, we first separately diagnose upward and downward LW radiative flux perturbations caused by an increase of CO2 alone. We find the following: 1) The change in downward LW flux contributes at least as much to the CO2 radiative cooling in the upper stratosphere as the change in upward LW flux; 2) the increasing with height temperature profile of the stratosphere results in a cooling due to the change in upward LW flux and a warming in the lower stratosphere due to the change in downward LW flux, which can offset or even overturn the cooling due to changes in upward LW flux.