|
Read Full Article (file size: 213167 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 108, NO. D12,
8517,
doi:10.1029/2002JD002598,
2003
A model study of stratospheric ozone in the troposphere and its contribution to tropospheric OH formation
A. S. Kentarchos
Institute for Marine and Atmospheric Research Utrecht (IMAU),
Utrecht University,
Utrecht,
Netherlands
G. J. Roelofs
Institute for Marine and Atmospheric Research Utrecht (IMAU),
Utrecht University,
Utrecht,
Netherlands
Abstract
Results from an 11-year simulation of the present-day atmosphere with a coupled tropospheric chemistry-climate model have
been used to investigate the extratropical transport from the stratosphere to the troposphere, the transport and photochemical
destruction of ozone from stratospheric origin in the troposphere, and the resulting contribution to tropospheric OH. The
simulated stratosphere–troposphere exchange (STE) is based on the model calculated wind fields, and its seasonality and spatial
distribution resemble results derived from other methods. The lifetime of stratospheric ozone in the troposphere is largely
determined by transport between the extratropical tropopause where it enters the troposphere and the subtropical lower troposphere
where its photochemical destruction rate maximizes. Comparison of the simulated ozone and O3s budgets suggests that ozone from stratospheric origin contributes about 15% to the average oxidation capacity in the Northern
Hemisphere (NH), with regional contributions up to 40%. STE has a reverse effect on OH in the extratropical upper troposphere
related to the influence of water vapor concentrations. The oxidation capacity of the troposphere may therefore be sensitive
to atmospheric dynamic effects of climate change.
Published 27
February
2003.
Index Terms: 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry; 3319 Meteorology and Atmospheric Dynamics: General circulation; 3337 Meteorology and Atmospheric Dynamics: Numerical modeling and data assimilation; 3362 Meteorology and Atmospheric Dynamics: Stratosphere/troposphere interactions.
Read Full Article (file size: 213167 bytes) Cited by
Citation: Kentarchos, A. S., and G. J. Roelofs
(2003),
A model study of stratospheric ozone in the troposphere and its contribution to tropospheric OH formation,
J. Geophys. Res.,
108(D12),
8517,
doi:10.1029/2002JD002598.
Copyright 2003 by the American Geophysical Union.
|