Journal articles
Basic features of large-scale processes in the middle atmosphere during DYANA
I.V. Bugaeva
1
A.I. Boutko
1
G.A. Kokin
1
Yu.P. Koshelkov
1
S.P. Perov
1
D.A. Tarasenko
1
G.R. Zakharov
1
G.F. Toulinov
2
D. Offermann
3
M. Bittner
3
U. von Zahn
4
Marie-Lise Chanin
5
Alain Hauchecorne
5
I. Soule
6
B.H. Subbaraya
7
M. Gil-Ojeda
8
B.A. de la Morena
F.J. Schmidlin
9
K.I. Oyama
10
H. Kanzawa
11
1
CAO - Central Aerological Observatory (Dolgoprudny, Moscow region, 141700 Russia - Russia)
2
IGA - Fedorov Institute of Applied Geophysics (Rostokinskaya 9, 129128, Moscow, Russia - Russia)
3
Bergische Universität Wuppertal (Gaußstraße 20, 42119 Wuppertal - Germany)
4
Rheinische Friedrich-Wilhelms-Universität Bonn (Regina-Pacis-Weg 3, 53113 Bonn - Germany)
5
SA - Service d'aéronomie (France)
- CNRS - Centre National de la Recherche Scientifique : UMR7620 (France)
- INSU - CNRS - Institut national des sciences de l'Univers (INSU-CNRS 3 rue Michel-Ange, 75794 Paris Cedex 16 - France)
- UPMC - Université Pierre et Marie Curie - Paris 6 (4 place Jussieu - 75005 Paris - France)
- UVSQ - Université de Versailles Saint-Quentin-en-Yvelines (55 avenue de Paris - 78035 Versailles cedex - France)
6
CFB - Canadian Forces Base (Cold Lake - Canada)
7
PRL - Physical Research Laboratory [Ahmedabad] (Navrangpura, Ahmedabad, Gujarat 380009 - India)
- ISRO - Indian Space Research Organisation (Bangalore - India)
8
INTA - Instituto Nacional de Técnica Aeroespacial ( Torrejón de Ardoz, Madrid - Spain)
9
GSFC - NASA Goddard Space Flight Center (Greenbelt, MD 20771 - United States)
10
ISAS - Institute of Space and Astronautical Science (Sagamihara City, Kanagawa Prefecture 252-5210 - Japan)
- JAXA - Japan Aerospace Exploration Agency [Sagamihara] (Chuo Ku, Sagamihara, Kanagawa 2525210, Japan - Japan)
11
NiPR - National Institute of Polar Research [Tokyo] (10-3 Midori-cho, Tachikawa-shi, Tokyo, 190-8518 - Japan)
Abstract : Large-scale processes in the stratosphere and mesosphere were investigated for the DYANA period, mainly on the basis of rocket sounding series and satellite-based maps. It was found that undisturbed circulation prevailed during the early winter period with low stratospheric temperatures near the Pole. Periodic warm pulses appeared in January in the upper stratosphere and an interrse warming was observed at these levels in early February, the downward penetration of which (below 25–30 km) was relatively confined. Wavenumber 1 predominated during the warming. In late February the cold cyclonic vortex was restored near the Pole and this persisted into March.
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Journal articles
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https://hal-insu.archives-ouvertes.fr/insu-03598727
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Submitted on : Saturday, March 5, 2022 - 8:45:37 PM
Last modification on : Monday, March 7, 2022 - 3:27:45 AM
Contributor : Catherine Cardon Connect in order to contact the contributor
Submitted on : Saturday, March 5, 2022 - 8:45:37 PM
Last modification on : Monday, March 7, 2022 - 3:27:45 AM
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- HAL Id : insu-03598727, version 1
- DOI : 10.1016/0021-9169(94)90003-5
Citation
I.V. Bugaeva, A.I. Boutko, G.A. Kokin, Yu.P. Koshelkov, S.P. Perov, et al.. Basic features of large-scale processes in the middle atmosphere during DYANA. Journal of Atmospheric and Terrestrial Physics, Elsevier, 1994, 56 (13-14), pp.1659-1674. ⟨10.1016/0021-9169(94)90003-5⟩. ⟨insu-03598727⟩
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