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GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 2,
1100,
doi:10.1029/2002GL016285,
2003
Fresh air in the 21st century?
Michael Prather
Department of Earth System Science,
UC Irvine,
California,
USA
Michael Gauss
Institutt for Geofysikk,
University of Oslo,
Oslo,
Norway
Terje Berntsen
Institutt for Geofysikk,
University of Oslo,
Oslo,
Norway
Ivar Isaksen
Institutt for Geofysikk,
University of Oslo,
Oslo,
Norway
Jostein Sundet
Institutt for Geofysikk,
University of Oslo,
Oslo,
Norway
Isabelle Bey
Swiss Federal Institute of Technology,
Lausanne,
Switzerland
Guy Brasseur
Max Planck Institute for Meteorology,
Hamburg,
Germany
Frank Dentener
Joint Research Centre, Environment Institute,
Ispra,
Italy
Richard Derwent
The Hadley Centre, UK Met Office,
Bracknell,
United Kingdom
David Stevenson
The Hadley Centre, UK Met Office,
Bracknell,
United Kingdom
Lee Grenfell
Didier Hauglustaine
Institut Pierre Simon Laplace,
CEA-CNRS,
Gif-sur-Yvette,
France
Larry Horowitz
Geophysical Fluid Dynamics Laboratory,
NOAA,
Princeton,
New Jersey,
USA
Daniel Jacob
Dept of Earth & Planetary Sciences,
Harvard U.,
Cambridge,
Maryland,
USA
Loretta Mickley
Dept of Earth & Planetary Sciences,
Harvard U.,
Cambridge,
Maryland,
USA
Mark Lawrence
Max Planck Institute for Chemistry,
Mainz,
Germany
Rolf von Kuhlmann
Max Planck Institute for Chemistry,
Mainz,
Germany
Jean-Francois Muller
Belgian Institute for Space Aeronomy,
Brussels,
Belgium
Giovanni Pitari
Dipartimento di Fisica, U.L'Aquila,
Coppito, L'Aquila,
Italy
Helen Rogers
Centre for Atmos. Sci.,
Cambridge U.,
Cambridge,
United Kingdom
Matthew Johnson
Centre for Atmos. Sci.,
Cambridge U.,
Cambridge,
United Kingdom
John Pyle
Centre for Atmos. Sci.,
Cambridge U.,
Cambridge,
United Kingdom
Kathy Law
Centre for Atmos. Sci.,
Cambridge U.,
Cambridge,
United Kingdom
Michiel van Weele
Royal Netherlands Meteorological Inst.,
De Bilt,
The Netherlands
Oliver Wild
Frontier Research System for Global Change,
Yokohama,
Japan
Abstract
Ozone is an air quality problem today for much of the world's population. Regions can exceed the ozone air quality standards
(AQS) through a combination of local emissions, meteorology favoring pollution episodes, and the clean-air baseline levels
of ozone upon which pollution builds. The IPCC 2001 assessment studied a range of global emission scenarios and found that
all but one projects increases in global tropospheric ozone during the 21st century. By 2030, near-surface increases over
much of the northern hemisphere are estimated to be about 5 ppb (+2 to +7 ppb over the range of scenarios). By 2100 the two
more extreme scenarios project baseline ozone increases of >20 ppb, while the other four scenarios give changes of −4 to +10
ppb. Even modest increases in the background abundance of tropospheric ozone might defeat current AQS strategies. The larger
increases, however, would gravely threaten both urban and rural air quality over most of the northern hemisphere.
Published 31
January
2003.
Index Terms: 0345 Atmospheric Composition and Structure: Pollution—urban and regional (0305); 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry; 1610 Global Change: Atmosphere (0315, 0325).
Read Full Article (file size: 277189 bytes) Cited by
Citation: Prather, M., et al.
(2003),
Fresh air in the 21st century?,
Geophys. Res. Lett.,
30(2),
1100,
doi:10.1029/2002GL016285.
Copyright 2003 by the American Geophysical Union.
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