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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).


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Citation: Prather, M., et al. (2003), Fresh air in the 21st century?, Geophys. Res. Lett., 30(2), 1100, doi:10.1029/2002GL016285.