Unprecedented evidence for deep convection hydrating the tropical stratosphere-Reference-Cited by-同舟云学术

Unprecedented evidence for deep convection hydrating the tropical stratosphere

Published:2008-05 Issue:10 Volume:35 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Corti T.¹,Luo B. P.¹,de Reus M.²,Brunner D.³,Cairo F.⁴,Mahoney M. J.⁵,Martucci G.⁶,Matthey R.⁷,Mitev V.⁷,dos Santos F. H.⁸,Schiller C.⁸,Shur G.⁹,Sitnikov N. M.⁹,Spelten N.⁸,Vössing H. J.²,Borrmann S.²¹⁰,Peter T.¹

Affiliation:

1. Institute for Atmospheric and Climate Science; ETH Zurich; Zurich Switzerland

2. Institute for Atmospheric Physics; Johannes-Gutenberg-University; Mainz Germany

3. Laboratory for Air Pollution and Environmental Technology; EMPA; Dübendorf Switzerland

4. Istituto di Scienze dell'Atmosfera e del Clima; Consiglio Nazionale delle Ricerche; Rome Italy

5. Jet Propulsion Laboratory; California Institute of Technology; Pasadena California USA

6. Consorzio Venezia Ricerche; Venice Italy

7. Centre Suisse d'Electronique et de Microtechnique SA (CSEM); Neuchatel Switzerland

8. Institute for Stratospheric Research; Forschungszentrum Jlich; Jlich Germany

9. Central Aerological Observatory; Moscow Russia

10. Particle Chemistry Department; Max-Planck-Institute for Chemistry; Mainz Germany

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2008GL033641/fullpdf

Reference23 articles.

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

3. A numerical study of tropical cross-tropopause transport by convective overshoots;Chaboureau;Atmos. Chem. Phys.,2007

4. The impact of cirrus clouds on tropical troposphere-to-stratosphere transport;Corti;Atmos. Chem. Phys.,2006

5. In situ evidence of rapid, vertical, irreversible transport of lower tropospheric air into the lower tropical stratosphere by convective cloud turrets and by larger-scale upwelling in tropical cyclones;Danielsen;J. Geophys. Res.,1993

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