1 Dynamical Polar Warming Amplification and a New Climate Feedback Analysis Framework Ming Cai Florida State University Tallahassee, FL 32306 [email protected].
Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.
Is Arctic Warming Causing Extremes in Mid-Latitude Weather? Florence Chen, Joseph Lanzillo, Upasna Sharma.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 11: 05/04/2010 ATM S 111, Global Warming: Understanding the Forecast.
Climate Sensitivity & Climate Feedback Instructor: Prof. Johnny Luo luo.
PTYS 214 – Spring 2011 Homework #5 available for download at the class websi te DUE Thursday, Feb. 24 Reminder: Extra Credit Presentations (up to 10pts)
Annual-mean TOA radiation (ERBE, W/m 2 ) Absorbed SW Outgoing LW.
Evidence for Milankovitch theory (wikipedia!). Px272 Lect 3: Forcing and feedback Balance of solar incoming, and earth emitted outgoing radiation Increments.
Overview II: Importance of the atmospheric boundary layer.
Chapter 15 Human Influences on Climate. Figure CO: Chapter 15, Human Influences on Climate--Air pollution in New York City © Dean D. Fetterolf/ShutterStock,
