Departure from Clausius-Clapeyron scaling of water entering the stratosphere in response to changes in tropical upwelling-Reference-Cited by-同舟云学术

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Departure from Clausius-Clapeyron scaling of water entering the stratosphere in response to changes in tropical upwelling

Published:2014-02-25 Issue:4 Volume:119 Page:1962-1972
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Fueglistaler S.¹,Liu Y. S.²,Flannaghan T. J.¹,Ploeger F.³,Haynes P. H.⁴

Affiliation:

1. Department of Geosciences/AOS; Princeton University; Princeton New Jersey USA

2. School of Geosciences; University of Edinburgh; Edinburgh UK

3. Institute of Energy and Climate Research, Stratosphere (IEK-7); Forschungszentrum Juelich; Juelich Germany

4. Department of Applied Mathematics and Theoretical Physics; University of Cambridge; Cambridge UK

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2013JD020772/fullpdf

Reference38 articles.

1. Photochemical evolution of ozone in the lower tropical stratosphere;Avallone;J. Geophys. Res.,1996

2. Seasonal differences of vertical-transport efficiency in the tropical tropopause layer: On the interplay between tropical deep convection, large-scale vertical ascent, and horizontal circulations;Bergman;J. Geophys. Res.,2012

3. A trajectory-based study of the tropical tropopause region;Bonazzola;J. Geophys. Res.,2004

4. Evidence for a world circulation provided by the measurements of helium and water vapor distribution in the stratosphere;Brewer;Q. J. R. Meteorol. Soc.,1949

5. Chemistry-climate model simulations of twenty-first century stratospheric climate and circulation changes;Butchart;J. Clim.,2010

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