Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring

We interpret observations from the Intercontinental Chemical Transport Experiment, Phase B (INTEX-B) in spring 2006 using a global chemical transport model (GEOS-Chem) to evaluate sensitivities of the free troposphere above the North Pacific Ocean and North America to Asian anthropogenic emissions....

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Main Authors: T. W. Walker, R. V. Martin, A. van Donkelaar, W. R. Leaitch, A. M. MacDonald, K. G. Anlauf, R. C. Cohen, T. H. Bertram, L. G. Huey, M. A. Avery, A. J. Weinheimer, F. M. Flocke, D. W. Tarasick, A. M. Thompson, D. G. Streets, X. Liu
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/8353/2010/acp-10-8353-2010.pdf
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author T. W. Walker
R. V. Martin
A. van Donkelaar
W. R. Leaitch
A. M. MacDonald
K. G. Anlauf
R. C. Cohen
T. H. Bertram
L. G. Huey
M. A. Avery
A. J. Weinheimer
F. M. Flocke
D. W. Tarasick
A. M. Thompson
D. G. Streets
X. Liu
author_facet T. W. Walker
R. V. Martin
A. van Donkelaar
W. R. Leaitch
A. M. MacDonald
K. G. Anlauf
R. C. Cohen
T. H. Bertram
L. G. Huey
M. A. Avery
A. J. Weinheimer
F. M. Flocke
D. W. Tarasick
A. M. Thompson
D. G. Streets
X. Liu
author_sort T. W. Walker
collection DOAJ
description We interpret observations from the Intercontinental Chemical Transport Experiment, Phase B (INTEX-B) in spring 2006 using a global chemical transport model (GEOS-Chem) to evaluate sensitivities of the free troposphere above the North Pacific Ocean and North America to Asian anthropogenic emissions. We develop a method to use satellite observations of tropospheric NO<sub>2</sub> columns to provide timely estimates of trends in NO<sub>x</sub> emissions. NO<sub>x</sub> emissions increased by 33% for China and 29% for East Asia from 2003 to 2006. We examine measurements from three aircraft platforms from the INTEX-B campaign, including a Canadian Cessna taking vertical profiles of ozone near Whistler Peak. The contribution to the mean simulated ozone profiles over Whistler below 5.5 km is at least 7.2 ppbv for Asian anthropogenic emissions and at least 3.5 ppbv for global lightning NO<sub>x</sub> emissions. Tropospheric ozone columns from OMI exhibit a broad Asian outflow plume across the Pacific, which is reproduced by simulation. Mean modelled sensitivities of Pacific (30° N–60° N) tropospheric ozone columns are at least 4.6 DU for Asian anthropogenic emissions and at least 3.3 DU for lightning, as determined by simulations excluding either source. Enhancements of ozone over Canada from Asian anthropogenic emissions reflect a combination of trans-Pacific transport of ozone produced over Asia, and ozone produced in the eastern Pacific through decomposition of peroxyacetyl nitrates (PANs). A sensitivity study decoupling PANs globally from the model's chemical mechanism establishes that PANs increase ozone production by removing NO<sub>x</sub> from regions of low ozone production efficiency (OPE) and injecting it into regions with higher OPE, resulting in a global increase in ozone production by 2% in spring 2006. PANs contribute up to 4 ppbv to surface springtime ozone concentrations in western Canada. Ozone production due to PAN transport is greatest in the eastern Pacific; commonly occurring transport patterns advect this ozone northeastward into Canada. Transport events observed by the aircraft confirm that polluted airmasses were advected in this way.
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spelling doaj.art-1194c4c66b3f42e195b5be2eb27aeb202022-12-22T02:41:03ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-09-0110178353837210.5194/acp-10-8353-2010Trans-Pacific transport of reactive nitrogen and ozone to Canada during springT. W. WalkerR. V. MartinA. van DonkelaarW. R. LeaitchA. M. MacDonaldK. G. AnlaufR. C. CohenT. H. BertramL. G. HueyM. A. AveryA. J. WeinheimerF. M. FlockeD. W. TarasickA. M. ThompsonD. G. StreetsX. LiuWe interpret observations from the Intercontinental Chemical Transport Experiment, Phase B (INTEX-B) in spring 2006 using a global chemical transport model (GEOS-Chem) to evaluate sensitivities of the free troposphere above the North Pacific Ocean and North America to Asian anthropogenic emissions. We develop a method to use satellite observations of tropospheric NO<sub>2</sub> columns to provide timely estimates of trends in NO<sub>x</sub> emissions. NO<sub>x</sub> emissions increased by 33% for China and 29% for East Asia from 2003 to 2006. We examine measurements from three aircraft platforms from the INTEX-B campaign, including a Canadian Cessna taking vertical profiles of ozone near Whistler Peak. The contribution to the mean simulated ozone profiles over Whistler below 5.5 km is at least 7.2 ppbv for Asian anthropogenic emissions and at least 3.5 ppbv for global lightning NO<sub>x</sub> emissions. Tropospheric ozone columns from OMI exhibit a broad Asian outflow plume across the Pacific, which is reproduced by simulation. Mean modelled sensitivities of Pacific (30° N–60° N) tropospheric ozone columns are at least 4.6 DU for Asian anthropogenic emissions and at least 3.3 DU for lightning, as determined by simulations excluding either source. Enhancements of ozone over Canada from Asian anthropogenic emissions reflect a combination of trans-Pacific transport of ozone produced over Asia, and ozone produced in the eastern Pacific through decomposition of peroxyacetyl nitrates (PANs). A sensitivity study decoupling PANs globally from the model's chemical mechanism establishes that PANs increase ozone production by removing NO<sub>x</sub> from regions of low ozone production efficiency (OPE) and injecting it into regions with higher OPE, resulting in a global increase in ozone production by 2% in spring 2006. PANs contribute up to 4 ppbv to surface springtime ozone concentrations in western Canada. Ozone production due to PAN transport is greatest in the eastern Pacific; commonly occurring transport patterns advect this ozone northeastward into Canada. Transport events observed by the aircraft confirm that polluted airmasses were advected in this way.http://www.atmos-chem-phys.net/10/8353/2010/acp-10-8353-2010.pdf
spellingShingle T. W. Walker
R. V. Martin
A. van Donkelaar
W. R. Leaitch
A. M. MacDonald
K. G. Anlauf
R. C. Cohen
T. H. Bertram
L. G. Huey
M. A. Avery
A. J. Weinheimer
F. M. Flocke
D. W. Tarasick
A. M. Thompson
D. G. Streets
X. Liu
Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
Atmospheric Chemistry and Physics
title Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
title_full Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
title_fullStr Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
title_full_unstemmed Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
title_short Trans-Pacific transport of reactive nitrogen and ozone to Canada during spring
title_sort trans pacific transport of reactive nitrogen and ozone to canada during spring
url http://www.atmos-chem-phys.net/10/8353/2010/acp-10-8353-2010.pdf
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