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AGU: Journal of Geophysical Research, Atmospheres

 

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  • Global Change: Atmosphere
  • Atmospheric Composition and Structure: Middle atmosphere—composition and chemistry
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Abstract
Cited By (5)
 

Abstract

Ozone loss from quasi-conservative coordinate mapping during the 1999–2000 SOLVE/THESEO 2000 campaigns

L. R. Lait

Science Systems and Applications, Inc., Lanham, Maryland, USA

M. R. Schoeberl

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

P. A. Newman

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

T. McGee

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

J. Burris

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

E. V. Browell

NASA Langley Research Center, Hampton, Virginia, USA

E. Richard

NOAA Aeronomy Laboratory and University of Colorado, Boulder, Colorado, USA

G. O. Braathen

Norwegian Institute for Air Research, Norway

B. R. Bojkov

Norwegian Institute for Air Research, Norway

F. Goutail

Centre National de la Recherche Scientifique, France

P. von der Gathen

Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany

E. Kyrö

Finnish Meteorological Institute, Sodankyla, Finland

G. Vaughan

University of Wales, Aberystwyth, UK

H. Kelder

Royal Netherlands Meteorological Institute (KNMI), De Bilt, Netherlands

S. Kirkwood

Swedish Institute of Space Physics, Sweden

P. Woods

National Physical Laboratory, UK

V. Dorokhov

Central Aerological Observatory, Moscow, Russia

I. Zaitcev

Central Aerological Observatory, Moscow, Russia

Z. Litynska

Institute of Meteorology and Water Management, Legionowo, Poland

B. Kois

Institute of Meteorology and Water Management, Legionowo, Poland

A. Benesova

Czech Hydrometeorological Institute (CHMI), Prague, Czech Republic

P. Skrivankova

Czech Hydrometeorological Institute (CHMI), Prague, Czech Republic

H. De Backer

Royal Meteorological Institute of Belgium (KMI/IRM), Belgium

J. Davies

Meteorological Service of Canada, Ontario, Canada

T. Jorgensen

Danish Meteorological Institute, Copenhagen, Denmark

I. S. Mikkelsen

Danish Meteorological Institute, Copenhagen, Denmark

Ozone observations made by the Airborne Raman Ozone, Temperature, and Aerosol Lidar (AROTEL) and Differential Absorption Lidar (DIAL) on board the NASA DC-8 aircraft, the NOAA in situ instrument on board the NASA ER-2 aircraft, and Third European Stratospheric Experiment on Ozone 2000 (THESEO 2000) ozonesondes are analyzed by applying a quasi-conservative coordinate mapping technique. Measurements from the late winter/early spring SAGE III Ozone Loss and Validation Experiment (SOLVE) period (January through March 2000) are incorporated into a time-varying composite field in a potential vorticity-potential temperature coordinate space; ozone loss rates are calculated both with and without diabatic effects. The average loss rate from mid-January to mid-March near the 450 K isentropic surface in the polar vortex is found to be approximately 0.03 ppmv/d.

Published 12 September 2002.

Citation: Lait, L. R., et al. (2002), Ozone loss from quasi-conservative coordinate mapping during the 1999–2000 SOLVE/THESEO 2000 campaigns, J. Geophys. Res., 107(D20), 8274, doi:10.1029/2001JD000998.

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