The response of midlatitude jets to increased CO2 : Distinguishing the roles of sea surface temperature and direct radiative forcing-Reference-Cited by-同舟云学术

The response of midlatitude jets to increased CO2 : Distinguishing the roles of sea surface temperature and direct radiative forcing

Published:2014-10-03 Issue:19 Volume:41 Page:6863-6871
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Grise Kevin M.¹,Polvani Lorenzo M.²³

Affiliation:

1. Department of Environmental Sciences; University of Virginia; Charlottesville Virginia USA

2. Lamont-Doherty Earth Observatory; Columbia University; Palisades New York USA

3. Department of Applied Physics and Applied Mathematics, and Department of Earth and Environmental Sciences; Columbia University; New York New York USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL061638/fullpdf

Reference21 articles.

1. Response of the midlatitude jets and of their variability to increased greenhouse gases in CMIP5 models;Barnes;J. Clim.,2013

2. Delayed Southern Hemisphere climate change induced by stratospheric ozone recovery, as projected by the CMIP5 models;Barnes;J. Clim.,2014

3. Opposite CMIP3/CMIP5 trends in the wintertime Northern Annular Mode explained by combined local sea ice and remote tropical influences;Cattiaux;Geophys. Res. Lett.,2013

4. Sensitivities of zonal mean atmospheric circulation to SST warming in an aqua-planet model;Chen;Geophys. Res. Lett.,2010

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