http://www.cnr.it/ontology/cnr/individuo/prodotto/ID45379
Unprecedented evidence for deep convection hydrating the tropical stratosphere (Articolo in rivista)
- Type
- Label
- Unprecedented evidence for deep convection hydrating the tropical stratosphere (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1029/2008GL033641 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- T. Corti (1); B. P. Luo (1); M. de Reus (2); D. Brunner (3); F. Cairo (4); M. J. Mahoney (5); G. Martucci (6); R. Matthey (7); V. Mitev (7); F. H. dos Santos (8); C. Schiller (8); G. Shur (9); N. M. Sitnikov (9); N. Spelten (8); H. J. Vössing (2); S. Borrmann (2)(10); T. Peter (1) (literal)
- Pagina inizio
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- Scopu (literal)
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 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, Du¨bendorf, 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. (literal)
- Titolo
- Unprecedented evidence for deep convection hydrating the tropical stratosphere (literal)
- Abstract
- We report on in situ and remote sensing measurements
of ice particles in the tropical stratosphere found during the
Geophysica campaigns TROCCINOX and SCOUT-O3. We
show that the deep convective systems penetrated the
stratosphere and deposited ice particles at altitudes reaching
420 K potential temperature. These convective events had a
hydrating effect on the lower tropical stratosphere due to
evaporation of the ice particles. In contrast, there were no
signs of convectively induced dehydration in the
stratosphere. (literal)
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