Abstract
Ozone loss from quasi-conservative coordinate mapping during the 1999–2000 SOLVE/THESEO 2000 campaigns
Science Systems and Applications, Inc., Lanham, Maryland, USA
NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
NASA Langley Research Center, Hampton, Virginia, USA
NOAA Aeronomy Laboratory and University of Colorado, Boulder, Colorado, USA
Norwegian Institute for Air Research, Norway
Norwegian Institute for Air Research, Norway
Centre National de la Recherche Scientifique, France
Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany
Finnish Meteorological Institute, Sodankyla, Finland
University of Wales, Aberystwyth, UK
Royal Netherlands Meteorological Institute (KNMI), De Bilt, Netherlands
Swedish Institute of Space Physics, Sweden
National Physical Laboratory, UK
Central Aerological Observatory, Moscow, Russia
Central Aerological Observatory, Moscow, Russia
Institute of Meteorology and Water Management, Legionowo, Poland
Institute of Meteorology and Water Management, Legionowo, Poland
Czech Hydrometeorological Institute (CHMI), Prague, Czech Republic
Czech Hydrometeorological Institute (CHMI), Prague, Czech Republic
Royal Meteorological Institute of Belgium (KMI/IRM), Belgium
Meteorological Service of Canada, Ontario, Canada
Danish Meteorological Institute, Copenhagen, Denmark
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: (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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