Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer-Reference-Cited by-同舟云学术

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Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer

Published:2013-07-27 Issue:14 Volume:118 Page:8111-8127
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Ploeger F.¹,Günther G.¹,Konopka P.¹,Fueglistaler S.²,Müller R.¹,Hoppe C.¹,Kunz A.¹³,Spang R.¹,Grooß J.-U.¹,Riese M.¹

Affiliation:

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

2. Department of Geosciences; Princeton University; Princeton New Jersey USA

3. Institute for Atmospheric and Climate Science; ETH Zuerich; Zuerich Switzerland

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/jgrd.50636/fullpdf

Reference81 articles.

1. Variability in upwelling across the tropical tropopause and correlations with tracers in the lower stratosphere;Abalos;Atmos. Chem. Phys.,2012

2. UV dosage levels in summer: Increased risk of ozone loss from convectively injected water vapor;Anderson;Science,2012

3. The role of the south-east Asian monsoon and other seasonal features in creating the “tape-recorder” signal in the Unified Model;Bannister;Q. J. R. Meteorol. Soc.,2004

4. A Lagrangian perspective of the tropopause and the ventilation of the lowermost stratosphere;Berthet;J. Geophys. Res.,2007

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