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Tiffany Shaw

Department of the Geophysical Sciences, University of Chicago

What does the seasonal cycle tell us about the atmospheric circulation response to global warming?

Room 811 AOSS, April 4, 2016, 3:30 PM

Abstract

The atmospheric circulation exhibits large seasonal changes between winter and summer that reflect the growth of the Monsoon. Here we exploit similarities between the present-day seasonal circulation changes and the projected circulation response to increased carbon dioxide (both are examples of direct radiative forcing) to understand future regional summertime circulation changes.



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