H.G. Brückelmann

University of Wuppertal

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D. Offermann

University of Wuppertal

K. U. Grossmann

University of Wuppertal

Ronald J. Thomas

New Mexico Institute of Mining and Technology

H. U. Widdel

Max Planck Institute for Solar System Research

K. Torkar

Institute of Oncology Ljubljana

P. Schwabbauer

University of Wuppertal

S. P. Perov

India Meteorological Department

P.H.G. Dickinson

Aerospace Technology Institute

P. Glöde

German Meteorological Service

D. Murtagh

Chalmers University of Technology

Cooperative Institutions

Roshydromet

Stockholm University

California Institute of Technology

Swedish Meteorological and Hydrological Institute

University of Wuppertal

NSF National Center for Atmospheric Research

Max Planck Society

German Meteorological Service

Centre National de la Recherche Scientifique

University of Bern

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Measurements of odd oxygen in the polar region on 10 February 1984 during MAP/WINE

Journal of Atmospheric and Terrestrial Physics (1987)

P.H.G. Dickinson G. Witt A. Zuber D. Murtagh K. U. Grossmann

Airglow

Mesopause

Rocket (weapon)

SCIAMACHY

10.1016/0021-9169(87)90023-7

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Citations (26)

Rocket-borne measurements of atmospheric infrared emissions by spectrometric techniques

Advances in Space Research (1987)

H.G. Brückelmann K. U. Grossmann D. Offermann

Zenith

Rocket (weapon)

10.1016/0273-1177(87)90074-3

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Citations (3)

Middle atmosphere abundances of water vapor and ozone during MAP/WINE

Journal of Atmospheric and Terrestrial Physics (1987)

K. U. Grossmann H.G. Brückelmann D. Offermann P. Schwabbauer R. Gyger

Mixing ratio

10.1016/0021-9169(87)90022-5

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Citations (18)

Mesopheric structure and the d-region winter anomaly

Advances in Space Research (1981)

D. Offermann H.G. Brückelmann K. Torkar H. U. Widdel

Anomaly (physics)

10.1016/0273-1177(81)90425-7

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Citations (4)

A scale analysis of the D region winter anomaly

Journal of Geophysical Research Atmospheres (1982)

D. Offermann H.G. Brückelmann J. J. Barnett K. Labitzke K. Torkar

A scale analysis, i.e., an estimation of typical values of important atmospheric and ionospheric parameters and time scales is performed for the meteorological type of winter anomaly at medium latitudes (40°N). An interpretative model of the winter anomaly is developed by a correlation analysis on the basis of data obtained from the Western European Winter Anomaly Campaign 1975/76 at El Arenosillo, Spain, and a simultaneous winter anomaly campaign at Wallops Island, U.S.A large number of rocket experiments performed in six previous winters in Spain are also analyzed and found to support the model. The model explains the buildup and decay of the winter anomaly by combined action of temperature, turbulent downward transport of nitric oxide, and horizontal transport of nitric oxide by winds. The horizontal wind direction is not important for the picture. Mechanisms involved are fast enough to explain the rapid variations of the winter anomaly. Large‐scale winter anomaly structure is linked to planetary wave number 2. The model picture is found to be compatible with quite a number of experimentally known features of the winter anomaly. There are hints to a more general validity of the model.

Anomaly (physics)

10.1029/ja087ia10p08286

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Citations (19)