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Ozone Trends in the Lower Stratosphere from Ozone Sondes Chemistry-Climate-Model simulations indicate that ozone in the mid-latitude lower troposphere should have generally been increasing since about 2000. Satellite data, however, have not confirmed such an increase. Instead, they seem to indicate that the pre-2000 decline of lower stratospheric ozone may have continued at mid-latitudes over the last 20 years as well [1,2]. Altitude resolution and information content of satellite observations on ozone in the lowermost stratosphere are, however, limited. Ozone sondes, on the other hand, provide the most detailed information on ozone in troposphere and lower stratosphere, but are limited to just a few soundings per month at maybe 40 stations world-wide [3].
Document ID
20210026799
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
W. Steinbrecht
(German Meteorological Service Offenbach, Germany)
R. Van Malderen
(Royal Meteorological Institute of Belgium Brussels, Belgium)
D. Poyraz
(Royal Meteorological Institute of Belgium Brussels, Belgium)
D. Hubert
(Royal Belgian Institute for Space Aeronomy (IASB-BIRA) Brussels, Belgium)
J. Davies
(Environment and Climate Change Canada Canada)
D.W. Tarasick
(Environment and Climate Change Canada Canada)
P. v. d. Gathen
(Alfred Wegener Institute for Polar and Marine Research Bremerhaven, Germany)
H. Deckelmann
(Alfred Wegener Institute for Polar and Marine Research Bremerhaven, Germany)
N. Jepsen
(Danish Meteorological Institute Copenhagen, Denmark)
R. Kivi
(Finnish Meteorological Institute Helsinki, Finland)
N. Lyall
(Met Office Exeter, United Kingdom)
B. Kois
(Institute of Meteorology and Water Management Warsaw, Poland)
P. Oelsner
(German Meteorological Service Offenbach, Germany)
M. Allaart
(Royal Netherlands Meteorological Institute De Bilt, Netherlands)
A. Piters
(Irish Met. Service)
M. Gill
(Met Éireann Dublin, Ireland)
G. Romanens
(MeteoSwiss Aerological Station Payerne, Switzerland)
R. Stübi
(MeteoSwiss Aerological Station Payerne, Switzerland)
G. Ancellet
(Atmospheres Laboratory Environments, Observations Spatiales Guyancourt, France)
S. Godin-Beekmann
(Atmospheres Laboratory Environments, Observations Spatiales Guyancourt, France)
B. Johnson
(Earth System Research Laboratory Boulder, Colorado, United States)
P. Cullis
(Earth System Research Laboratory Boulder, Colorado, United States)
I. Petropavlovskik
(Earth System Research Laboratory Boulder, Colorado, United States)
J.- L. Hernandez
(Agencia Estatal de Meteorología Madrid, Spain)
A. Diaz Rodriguez
(Agencia Estatal de Meteorología Madrid, Spain)
T. Nakano
(Japan Meteorological Agency Tokyo, Japan)
C. Torres
(Agencia Estatal de Meteorología Madrid, Spain)
M. Tully
(Bureau of Meteorology)
R. Querel
(National Institute of Water and Atmospheric Research Hamilton, New Zealand)
D. E. Kollonige
(Goddard Space Flight Center Greenbelt, Maryland, United States)
R. M. Stauffer
(Goddard Space Flight Center Greenbelt, Maryland, United States)
A.M. Thompson
(Goddard Space Flight Center Greenbelt, Maryland, United States)
K.- L. Chang
(Cooperative Institute for Research in Environmental Sciences Boulder, Colorado, United States)
O.R. Cooper
(Cooperative Institute for Research in Environmental Sciences Boulder, Colorado, United States)
H.G.J. Smit
(Forschungszentrum Jülich Jülich, Germany)
Date Acquired
January 12, 2022
Subject Category
Geosciences (General)
Meeting Information
Meeting: Quadrennial Ozone Symposium 2021
Location: Online
Country: KR
Start Date: October 3, 2021
End Date: October 9, 2021
Sponsors: Quadrennial Ozone Symposium 2021
Funding Number(s)
WBS: 281945.02.80.01.06
Distribution Limits
Public
Copyright
Portions of document may include copyright protected material.
Technical Review
NASA Peer Committee
Keywords
lower stratospheric ozone trends
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