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MICS-Asia II. Impact of global emissions on regional air quality in Asia

Identifieur interne : 000107 ( PascalFrancis/Corpus ); précédent : 000106; suivant : 000108

MICS-Asia II. Impact of global emissions on regional air quality in Asia

Auteurs : Tracey Holloway ; Tatsuya Sakurai ; ZHIWEI HAN ; Susanna Ehlers ; Scott N. Spak ; Larry W. Horowitz ; Gregory R. Carmichael ; David G. Streets ; Y. Hozumi ; Hiromasa Ueda ; S. U. Park ; Christopher Fung ; M. Kajino ; Narisara Thongboonchoo ; Magnuz Engardt ; Cecilia Bennet ; Hiroshi Hayami ; Karine Sartelet ; ZIFA WANG ; K. Matsuda ; Markus Amann

Source :

RBID : Pascal:08-0372728

Descripteurs français

English descriptors

Abstract

This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O3 contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O3, even for surface concentrations. Both North America and Europe contribute to ground-level O3 concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O3 during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O3 generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

pA  
A01 01  1    @0 1352-2310
A03   1    @0 Atmos. environ. : (1994)
A05       @2 42
A06       @2 15
A08 01  1  ENG  @1 MICS-Asia II. Impact of global emissions on regional air quality in Asia
A09 01  1  ENG  @1 MICS-ASIA II
A11 01  1    @1 HOLLOWAY (Tracey)
A11 02  1    @1 SAKURAI (Tatsuya)
A11 03  1    @1 ZHIWEI HAN
A11 04  1    @1 EHLERS (Susanna)
A11 05  1    @1 SPAK (Scott N.)
A11 06  1    @1 HOROWITZ (Larry W.)
A11 07  1    @1 CARMICHAEL (Gregory R.)
A11 08  1    @1 STREETS (David G.)
A11 09  1    @1 HOZUMI (Y.)
A11 10  1    @1 UEDA (Hiromasa)
A11 11  1    @1 PARK (S. U.)
A11 12  1    @1 FUNG (Christopher)
A11 13  1    @1 KAJINO (M.)
A11 14  1    @1 THONGBOONCHOO (Narisara)
A11 15  1    @1 ENGARDT (Magnuz)
A11 16  1    @1 BENNET (Cecilia)
A11 17  1    @1 HAYAMI (Hiroshi)
A11 18  1    @1 SARTELET (Karine)
A11 19  1    @1 ZIFA WANG
A11 20  1    @1 MATSUDA (K.)
A11 21  1    @1 AMANN (Markus)
A12 01  1    @1 CARMICHAEL (Gregory R.) @9 ed.
A12 02  1    @1 UEDA (Hiromasa) @9 ed.
A14 01      @1 Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A @2 Madison, WI 53726 @3 USA @Z 1 aut. @Z 4 aut. @Z 5 aut.
A14 02      @1 Acid Deposition and Oxidant Research Center @2 Niigata @3 JPN @Z 2 aut. @Z 3 aut. @Z 9 aut. @Z 10 aut.
A14 03      @1 Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS) @3 CHN @Z 3 aut.
A14 04      @1 NOAA Geophysical Fluid Dynamics Laboratory @2 Princeton, NJ @3 USA @Z 6 aut.
A14 05      @1 Center for Global and Regional Environmental Research, University of Iowa @2 IA @3 USA @Z 7 aut. @Z 14 aut.
A14 06      @1 Argonne National Laboratory @2 IL @3 USA @Z 8 aut.
A14 07      @1 Seoul National University @2 Seoul @3 KOR @Z 11 aut.
A14 08      @1 Hong Kong Environmental Protection Department @3 HKG @Z 12 aut.
A14 09      @1 Disaster Prevention Research Institute, Kyoto University @2 Kyoto @3 JPN @Z 13 aut.
A14 10      @1 Swedish Meteorological and Hydrological Institute @2 Norrkoping @3 SWE @Z 15 aut. @Z 16 aut.
A14 11      @1 Central Research Institute of Electric Power Industry @2 Chiba @3 JPN @Z 17 aut.
A14 12      @1 Centre d'Enseignement et de Recherche en Environnement Atmosphérique @3 FRA @Z 18 aut.
A14 13      @1 Institute of Atmospheric Physics @2 Beijing @3 CHN @Z 19 aut.
A14 14      @1 Meisei University @2 Tokyo @3 JPN @Z 20 aut.
A14 15      @1 International Institute for Applied System Analysis @2 Laxenburg @3 AUT @Z 21 aut.
A15 01      @1 Department of Chemical and Biochemical Engineering, Center for Global and Regional Environmental Research, University of Iowa @2 Iowa City, IA 52240 @3 USA @Z 1 aut.
A15 02      @1 Acid Deposition and Oxidant Research Center (ADORC), designated as Network Center for EANET (Acid Deposition Monitoring Network in East Asia) @3 JPN @Z 2 aut.
A20       @1 3543-3561
A21       @1 2008
A23 01      @0 ENG
A43 01      @1 INIST @2 8940B @5 354000183183120050
A44       @0 0000 @1 © 2008 INIST-CNRS. All rights reserved.
A45       @0 1 p.3/4
A47 01  1    @0 08-0372728
A60       @1 P
A61       @0 A
A64 01  1    @0 Atmospheric environment : (1994)
A66 01      @0 GBR
C01 01    ENG  @0 This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O3 contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O3, even for surface concentrations. Both North America and Europe contribute to ground-level O3 concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O3 during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O3 generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.
C02 01  X    @0 001D16C03
C03 01  X  FRE  @0 Troposphère @5 01
C03 01  X  ENG  @0 Troposphere @5 01
C03 01  X  SPA  @0 Troposfera @5 01
C03 02  X  FRE  @0 Qualité air @5 02
C03 02  X  ENG  @0 Air quality @5 02
C03 02  X  SPA  @0 Calidad aire @5 02
C03 03  X  FRE  @0 Echelon régional @5 03
C03 03  X  ENG  @0 Regional scope @5 03
C03 03  X  SPA  @0 Escala regional @5 03
C03 04  X  FRE  @0 Relation source puits @5 04
C03 04  X  ENG  @0 Source sink relationship @5 04
C03 04  X  SPA  @0 Relación fuente sumidero @5 04
C03 05  X  FRE  @0 Source pollution @5 05
C03 05  X  ENG  @0 Pollution source @5 05
C03 05  X  SPA  @0 Fuente polución @5 05
C03 06  X  FRE  @0 Phénomène transport @5 06
C03 06  X  ENG  @0 Transport process @5 06
C03 06  X  SPA  @0 Fenómeno transporte @5 06
C03 07  X  FRE  @0 Transport polluant grande distance @5 07
C03 07  X  ENG  @0 Long range pollutant transport @5 07
C03 07  X  SPA  @0 Transporte contaminante gran distancia @5 07
C03 08  X  FRE  @0 Variation saisonnière @5 08
C03 08  X  ENG  @0 Seasonal variation @5 08
C03 08  X  SPA  @0 Variación estacional @5 08
C03 09  X  FRE  @0 Variation spatiale @5 09
C03 09  X  ENG  @0 Spatial variation @5 09
C03 09  X  SPA  @0 Variación espacial @5 09
C03 10  X  FRE  @0 Ozone @2 NK @2 FX @5 10
C03 10  X  ENG  @0 Ozone @2 NK @2 FX @5 10
C03 10  X  SPA  @0 Ozono @2 NK @2 FX @5 10
C03 11  X  FRE  @0 Polluant secondaire @5 11
C03 11  X  ENG  @0 Secondary pollutant @5 11
C03 11  X  SPA  @0 Contaminante secundario @5 11
C03 12  X  FRE  @0 Composé trace @5 12
C03 12  X  ENG  @0 Trace compound @5 12
C03 12  X  SPA  @0 Compuesto huella @5 12
C03 13  X  FRE  @0 Monoxyde de carbone @2 NK @2 FX @5 13
C03 13  X  ENG  @0 Carbon monoxide @2 NK @2 FX @5 13
C03 13  X  SPA  @0 Carbono monóxido @2 NK @2 FX @5 13
C03 14  X  FRE  @0 Simulation numérique @5 14
C03 14  X  ENG  @0 Numerical simulation @5 14
C03 14  X  SPA  @0 Simulación numérica @5 14
C03 15  X  FRE  @0 Distribution concentration @5 15
C03 15  X  ENG  @0 Concentration distribution @5 15
C03 15  X  SPA  @0 Distribución concentración @5 15
C03 16  X  FRE  @0 Etude comparative @5 16
C03 16  X  ENG  @0 Comparative study @5 16
C03 16  X  SPA  @0 Estudio comparativo @5 16
C03 17  X  FRE  @0 Performance algorithme @5 17
C03 17  X  ENG  @0 Algorithm performance @5 17
C03 17  X  SPA  @0 Resultado algoritmo @5 17
C03 18  X  FRE  @0 Prévision pollution atmosphérique @5 18
C03 18  X  ENG  @0 Atmospheric pollution forecasting @5 18
C03 18  X  SPA  @0 Previsión contaminación del ambiente @5 18
C03 19  X  FRE  @0 Modèle prévision @5 19
C03 19  X  ENG  @0 Forecast model @5 19
C03 19  X  SPA  @0 Modelo previsión @5 19
C03 20  X  FRE  @0 Asie @2 NG @5 31
C03 20  X  ENG  @0 Asia @2 NG @5 31
C03 20  X  SPA  @0 Asia @2 NG @5 31
N21       @1 238

Format Inist (serveur)

NO : PASCAL 08-0372728 INIST
ET : MICS-Asia II. Impact of global emissions on regional air quality in Asia
AU : HOLLOWAY (Tracey); SAKURAI (Tatsuya); ZHIWEI HAN; EHLERS (Susanna); SPAK (Scott N.); HOROWITZ (Larry W.); CARMICHAEL (Gregory R.); STREETS (David G.); HOZUMI (Y.); UEDA (Hiromasa); PARK (S. U.); FUNG (Christopher); KAJINO (M.); THONGBOONCHOO (Narisara); ENGARDT (Magnuz); BENNET (Cecilia); HAYAMI (Hiroshi); SARTELET (Karine); ZIFA WANG; MATSUDA (K.); AMANN (Markus); CARMICHAEL (Gregory R.); UEDA (Hiromasa)
AF : Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A/Madison, WI 53726/Etats-Unis (1 aut., 4 aut., 5 aut.); Acid Deposition and Oxidant Research Center/Niigata/Japon (2 aut., 3 aut., 9 aut., 10 aut.); Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS)/Chine (3 aut.); NOAA Geophysical Fluid Dynamics Laboratory/Princeton, NJ/Etats-Unis (6 aut.); Center for Global and Regional Environmental Research, University of Iowa/IA/Etats-Unis (7 aut., 14 aut.); Argonne National Laboratory/IL/Etats-Unis (8 aut.); Seoul National University/Seoul/Corée, République de (11 aut.); Hong Kong Environmental Protection Department/Hong-Kong (12 aut.); Disaster Prevention Research Institute, Kyoto University/Kyoto/Japon (13 aut.); Swedish Meteorological and Hydrological Institute/Norrkoping/Suède (15 aut., 16 aut.); Central Research Institute of Electric Power Industry/Chiba/Japon (17 aut.); Centre d'Enseignement et de Recherche en Environnement Atmosphérique/France (18 aut.); Institute of Atmospheric Physics/Beijing/Chine (19 aut.); Meisei University/Tokyo/Japon (20 aut.); International Institute for Applied System Analysis/Laxenburg/Autriche (21 aut.); Department of Chemical and Biochemical Engineering, Center for Global and Regional Environmental Research, University of Iowa/Iowa City, IA 52240/Etats-Unis (1 aut.); Acid Deposition and Oxidant Research Center (ADORC), designated as Network Center for EANET (Acid Deposition Monitoring Network in East Asia)/Japon (2 aut.)
DT : Publication en série; Niveau analytique
SO : Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2008; Vol. 42; No. 15; Pp. 3543-3561; Bibl. 1 p.3/4
LA : Anglais
EA : This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O3 contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O3, even for surface concentrations. Both North America and Europe contribute to ground-level O3 concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O3 during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O3 generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.
CC : 001D16C03
FD : Troposphère; Qualité air; Echelon régional; Relation source puits; Source pollution; Phénomène transport; Transport polluant grande distance; Variation saisonnière; Variation spatiale; Ozone; Polluant secondaire; Composé trace; Monoxyde de carbone; Simulation numérique; Distribution concentration; Etude comparative; Performance algorithme; Prévision pollution atmosphérique; Modèle prévision; Asie
ED : Troposphere; Air quality; Regional scope; Source sink relationship; Pollution source; Transport process; Long range pollutant transport; Seasonal variation; Spatial variation; Ozone; Secondary pollutant; Trace compound; Carbon monoxide; Numerical simulation; Concentration distribution; Comparative study; Algorithm performance; Atmospheric pollution forecasting; Forecast model; Asia
SD : Troposfera; Calidad aire; Escala regional; Relación fuente sumidero; Fuente polución; Fenómeno transporte; Transporte contaminante gran distancia; Variación estacional; Variación espacial; Ozono; Contaminante secundario; Compuesto huella; Carbono monóxido; Simulación numérica; Distribución concentración; Estudio comparativo; Resultado algoritmo; Previsión contaminación del ambiente; Modelo previsión; Asia
LO : INIST-8940B.354000183183120050
ID : 08-0372728

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Pascal:08-0372728

Le document en format XML

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<name sortKey="Thongboonchoo, Narisara" sort="Thongboonchoo, Narisara" uniqKey="Thongboonchoo N" first="Narisara" last="Thongboonchoo">Narisara Thongboonchoo</name>
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</affiliation>
</author>
<author>
<name sortKey="Zifa Wang" sort="Zifa Wang" uniqKey="Zifa Wang" last="Zifa Wang">ZIFA WANG</name>
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<s1>Institute of Atmospheric Physics</s1>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Matsuda, K" sort="Matsuda, K" uniqKey="Matsuda K" first="K." last="Matsuda">K. Matsuda</name>
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<inist:fA14 i1="14">
<s1>Meisei University</s1>
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<sZ>20 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Amann, Markus" sort="Amann, Markus" uniqKey="Amann M" first="Markus" last="Amann">Markus Amann</name>
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<inist:fA14 i1="15">
<s1>International Institute for Applied System Analysis</s1>
<s2>Laxenburg</s2>
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<date when="2008">2008</date>
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<idno type="RBID">Pascal:08-0372728</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000107</idno>
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<title xml:lang="en" level="a">MICS-Asia II. Impact of global emissions on regional air quality in Asia</title>
<author>
<name sortKey="Holloway, Tracey" sort="Holloway, Tracey" uniqKey="Holloway T" first="Tracey" last="Holloway">Tracey Holloway</name>
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<s1>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A</s1>
<s2>Madison, WI 53726</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Sakurai, Tatsuya" sort="Sakurai, Tatsuya" uniqKey="Sakurai T" first="Tatsuya" last="Sakurai">Tatsuya Sakurai</name>
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</affiliation>
</author>
<author>
<name sortKey="Zhiwei Han" sort="Zhiwei Han" uniqKey="Zhiwei Han" last="Zhiwei Han">ZHIWEI HAN</name>
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<sZ>10 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation>
<inist:fA14 i1="03">
<s1>Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS)</s1>
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<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Ehlers, Susanna" sort="Ehlers, Susanna" uniqKey="Ehlers S" first="Susanna" last="Ehlers">Susanna Ehlers</name>
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<sZ>1 aut.</sZ>
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<name sortKey="Spak, Scott N" sort="Spak, Scott N" uniqKey="Spak S" first="Scott N." last="Spak">Scott N. Spak</name>
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<sZ>1 aut.</sZ>
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<name sortKey="Horowitz, Larry W" sort="Horowitz, Larry W" uniqKey="Horowitz L" first="Larry W." last="Horowitz">Larry W. Horowitz</name>
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</affiliation>
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<author>
<name sortKey="Carmichael, Gregory R" sort="Carmichael, Gregory R" uniqKey="Carmichael G" first="Gregory R." last="Carmichael">Gregory R. Carmichael</name>
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<inist:fA14 i1="05">
<s1>Center for Global and Regional Environmental Research, University of Iowa</s1>
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</inist:fA14>
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</author>
<author>
<name sortKey="Streets, David G" sort="Streets, David G" uniqKey="Streets D" first="David G." last="Streets">David G. Streets</name>
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<inist:fA14 i1="06">
<s1>Argonne National Laboratory</s1>
<s2>IL</s2>
<s3>USA</s3>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Hozumi, Y" sort="Hozumi, Y" uniqKey="Hozumi Y" first="Y." last="Hozumi">Y. Hozumi</name>
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<inist:fA14 i1="02">
<s1>Acid Deposition and Oxidant Research Center</s1>
<s2>Niigata</s2>
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<author>
<name sortKey="Ueda, Hiromasa" sort="Ueda, Hiromasa" uniqKey="Ueda H" first="Hiromasa" last="Ueda">Hiromasa Ueda</name>
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<inist:fA14 i1="02">
<s1>Acid Deposition and Oxidant Research Center</s1>
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</affiliation>
</author>
<author>
<name sortKey="Park, S U" sort="Park, S U" uniqKey="Park S" first="S. U." last="Park">S. U. Park</name>
<affiliation>
<inist:fA14 i1="07">
<s1>Seoul National University</s1>
<s2>Seoul</s2>
<s3>KOR</s3>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Fung, Christopher" sort="Fung, Christopher" uniqKey="Fung C" first="Christopher" last="Fung">Christopher Fung</name>
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<inist:fA14 i1="08">
<s1>Hong Kong Environmental Protection Department</s1>
<s3>HKG</s3>
<sZ>12 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Kajino, M" sort="Kajino, M" uniqKey="Kajino M" first="M." last="Kajino">M. Kajino</name>
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<inist:fA14 i1="09">
<s1>Disaster Prevention Research Institute, Kyoto University</s1>
<s2>Kyoto</s2>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Thongboonchoo, Narisara" sort="Thongboonchoo, Narisara" uniqKey="Thongboonchoo N" first="Narisara" last="Thongboonchoo">Narisara Thongboonchoo</name>
<affiliation>
<inist:fA14 i1="05">
<s1>Center for Global and Regional Environmental Research, University of Iowa</s1>
<s2>IA</s2>
<s3>USA</s3>
<sZ>7 aut.</sZ>
<sZ>14 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Engardt, Magnuz" sort="Engardt, Magnuz" uniqKey="Engardt M" first="Magnuz" last="Engardt">Magnuz Engardt</name>
<affiliation>
<inist:fA14 i1="10">
<s1>Swedish Meteorological and Hydrological Institute</s1>
<s2>Norrkoping</s2>
<s3>SWE</s3>
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<sZ>16 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Bennet, Cecilia" sort="Bennet, Cecilia" uniqKey="Bennet C" first="Cecilia" last="Bennet">Cecilia Bennet</name>
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<inist:fA14 i1="10">
<s1>Swedish Meteorological and Hydrological Institute</s1>
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<name sortKey="Hayami, Hiroshi" sort="Hayami, Hiroshi" uniqKey="Hayami H" first="Hiroshi" last="Hayami">Hiroshi Hayami</name>
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<inist:fA14 i1="11">
<s1>Central Research Institute of Electric Power Industry</s1>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Sartelet, Karine" sort="Sartelet, Karine" uniqKey="Sartelet K" first="Karine" last="Sartelet">Karine Sartelet</name>
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<inist:fA14 i1="12">
<s1>Centre d'Enseignement et de Recherche en Environnement Atmosphérique</s1>
<s3>FRA</s3>
<sZ>18 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Zifa Wang" sort="Zifa Wang" uniqKey="Zifa Wang" last="Zifa Wang">ZIFA WANG</name>
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<inist:fA14 i1="13">
<s1>Institute of Atmospheric Physics</s1>
<s2>Beijing</s2>
<s3>CHN</s3>
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</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Matsuda, K" sort="Matsuda, K" uniqKey="Matsuda K" first="K." last="Matsuda">K. Matsuda</name>
<affiliation>
<inist:fA14 i1="14">
<s1>Meisei University</s1>
<s2>Tokyo</s2>
<s3>JPN</s3>
<sZ>20 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author>
<name sortKey="Amann, Markus" sort="Amann, Markus" uniqKey="Amann M" first="Markus" last="Amann">Markus Amann</name>
<affiliation>
<inist:fA14 i1="15">
<s1>International Institute for Applied System Analysis</s1>
<s2>Laxenburg</s2>
<s3>AUT</s3>
<sZ>21 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
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<series>
<title level="j" type="main">Atmospheric environment : (1994)</title>
<title level="j" type="abbreviated">Atmos. environ. : (1994)</title>
<idno type="ISSN">1352-2310</idno>
<imprint>
<date when="2008">2008</date>
</imprint>
</series>
</biblStruct>
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<title level="j" type="main">Atmospheric environment : (1994)</title>
<title level="j" type="abbreviated">Atmos. environ. : (1994)</title>
<idno type="ISSN">1352-2310</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Air quality</term>
<term>Algorithm performance</term>
<term>Asia</term>
<term>Atmospheric pollution forecasting</term>
<term>Carbon monoxide</term>
<term>Comparative study</term>
<term>Concentration distribution</term>
<term>Forecast model</term>
<term>Long range pollutant transport</term>
<term>Numerical simulation</term>
<term>Ozone</term>
<term>Pollution source</term>
<term>Regional scope</term>
<term>Seasonal variation</term>
<term>Secondary pollutant</term>
<term>Source sink relationship</term>
<term>Spatial variation</term>
<term>Trace compound</term>
<term>Transport process</term>
<term>Troposphere</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Troposphère</term>
<term>Qualité air</term>
<term>Echelon régional</term>
<term>Relation source puits</term>
<term>Source pollution</term>
<term>Phénomène transport</term>
<term>Transport polluant grande distance</term>
<term>Variation saisonnière</term>
<term>Variation spatiale</term>
<term>Ozone</term>
<term>Polluant secondaire</term>
<term>Composé trace</term>
<term>Monoxyde de carbone</term>
<term>Simulation numérique</term>
<term>Distribution concentration</term>
<term>Etude comparative</term>
<term>Performance algorithme</term>
<term>Prévision pollution atmosphérique</term>
<term>Modèle prévision</term>
<term>Asie</term>
</keywords>
</textClass>
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</teiHeader>
<front>
<div type="abstract" xml:lang="en">This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O
<sub>3</sub>
contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O
<sub>3</sub>
, even for surface concentrations. Both North America and Europe contribute to ground-level O
<sub>3</sub>
concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O
<sub>3</sub>
during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O
<sub>3</sub>
generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.</div>
</front>
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<s1>SPAK (Scott N.)</s1>
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<s1>HOROWITZ (Larry W.)</s1>
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<s1>CARMICHAEL (Gregory R.)</s1>
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<s1>STREETS (David G.)</s1>
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<s1>HOZUMI (Y.)</s1>
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<s1>KAJINO (M.)</s1>
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<s1>ZIFA WANG</s1>
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<s1>MATSUDA (K.)</s1>
</fA11>
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<s1>AMANN (Markus)</s1>
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<fA12 i1="01" i2="1">
<s1>CARMICHAEL (Gregory R.)</s1>
<s9>ed.</s9>
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<s1>UEDA (Hiromasa)</s1>
<s9>ed.</s9>
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<s1>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A</s1>
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<sZ>1 aut.</sZ>
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<sZ>5 aut.</sZ>
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<s1>Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS)</s1>
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<sZ>3 aut.</sZ>
</fA14>
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<s1>NOAA Geophysical Fluid Dynamics Laboratory</s1>
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</fA14>
<fA14 i1="05">
<s1>Center for Global and Regional Environmental Research, University of Iowa</s1>
<s2>IA</s2>
<s3>USA</s3>
<sZ>7 aut.</sZ>
<sZ>14 aut.</sZ>
</fA14>
<fA14 i1="06">
<s1>Argonne National Laboratory</s1>
<s2>IL</s2>
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<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="07">
<s1>Seoul National University</s1>
<s2>Seoul</s2>
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<fA14 i1="08">
<s1>Hong Kong Environmental Protection Department</s1>
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<fA14 i1="09">
<s1>Disaster Prevention Research Institute, Kyoto University</s1>
<s2>Kyoto</s2>
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<s1>Swedish Meteorological and Hydrological Institute</s1>
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</fA14>
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<s1>Central Research Institute of Electric Power Industry</s1>
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</fA14>
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<s1>Centre d'Enseignement et de Recherche en Environnement Atmosphérique</s1>
<s3>FRA</s3>
<sZ>18 aut.</sZ>
</fA14>
<fA14 i1="13">
<s1>Institute of Atmospheric Physics</s1>
<s2>Beijing</s2>
<s3>CHN</s3>
<sZ>19 aut.</sZ>
</fA14>
<fA14 i1="14">
<s1>Meisei University</s1>
<s2>Tokyo</s2>
<s3>JPN</s3>
<sZ>20 aut.</sZ>
</fA14>
<fA14 i1="15">
<s1>International Institute for Applied System Analysis</s1>
<s2>Laxenburg</s2>
<s3>AUT</s3>
<sZ>21 aut.</sZ>
</fA14>
<fA15 i1="01">
<s1>Department of Chemical and Biochemical Engineering, Center for Global and Regional Environmental Research, University of Iowa</s1>
<s2>Iowa City, IA 52240</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
</fA15>
<fA15 i1="02">
<s1>Acid Deposition and Oxidant Research Center (ADORC), designated as Network Center for EANET (Acid Deposition Monitoring Network in East Asia)</s1>
<s3>JPN</s3>
<sZ>2 aut.</sZ>
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<s5>354000183183120050</s5>
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<s1>© 2008 INIST-CNRS. All rights reserved.</s1>
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<s0>08-0372728</s0>
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<fA60>
<s1>P</s1>
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<fA61>
<s0>A</s0>
</fA61>
<fA64 i1="01" i2="1">
<s0>Atmospheric environment : (1994)</s0>
</fA64>
<fA66 i1="01">
<s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG">
<s0>This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O
<sub>3</sub>
contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O
<sub>3</sub>
, even for surface concentrations. Both North America and Europe contribute to ground-level O
<sub>3</sub>
concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O
<sub>3</sub>
during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O
<sub>3</sub>
generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.</s0>
</fC01>
<fC02 i1="01" i2="X">
<s0>001D16C03</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE">
<s0>Troposphère</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG">
<s0>Troposphere</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA">
<s0>Troposfera</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE">
<s0>Qualité air</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG">
<s0>Air quality</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA">
<s0>Calidad aire</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE">
<s0>Echelon régional</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG">
<s0>Regional scope</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA">
<s0>Escala regional</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE">
<s0>Relation source puits</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG">
<s0>Source sink relationship</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA">
<s0>Relación fuente sumidero</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE">
<s0>Source pollution</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG">
<s0>Pollution source</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA">
<s0>Fuente polución</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE">
<s0>Phénomène transport</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Transport process</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Fenómeno transporte</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE">
<s0>Transport polluant grande distance</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG">
<s0>Long range pollutant transport</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA">
<s0>Transporte contaminante gran distancia</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Variation saisonnière</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Seasonal variation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Variación estacional</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE">
<s0>Variation spatiale</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG">
<s0>Spatial variation</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA">
<s0>Variación espacial</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Ozono</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Polluant secondaire</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>Secondary pollutant</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Contaminante secundario</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE">
<s0>Composé trace</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG">
<s0>Trace compound</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA">
<s0>Compuesto huella</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE">
<s0>Monoxyde de carbone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG">
<s0>Carbon monoxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA">
<s0>Carbono monóxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE">
<s0>Simulation numérique</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG">
<s0>Numerical simulation</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA">
<s0>Simulación numérica</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE">
<s0>Distribution concentration</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG">
<s0>Concentration distribution</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA">
<s0>Distribución concentración</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="X" l="FRE">
<s0>Etude comparative</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="X" l="ENG">
<s0>Comparative study</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="X" l="SPA">
<s0>Estudio comparativo</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE">
<s0>Performance algorithme</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG">
<s0>Algorithm performance</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA">
<s0>Resultado algoritmo</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="X" l="FRE">
<s0>Prévision pollution atmosphérique</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="ENG">
<s0>Atmospheric pollution forecasting</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="X" l="SPA">
<s0>Previsión contaminación del ambiente</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="X" l="FRE">
<s0>Modèle prévision</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="X" l="ENG">
<s0>Forecast model</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="X" l="SPA">
<s0>Modelo previsión</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="X" l="FRE">
<s0>Asie</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fC03 i1="20" i2="X" l="ENG">
<s0>Asia</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fC03 i1="20" i2="X" l="SPA">
<s0>Asia</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fN21>
<s1>238</s1>
</fN21>
</pA>
</standard>
<server>
<NO>PASCAL 08-0372728 INIST</NO>
<ET>MICS-Asia II. Impact of global emissions on regional air quality in Asia</ET>
<AU>HOLLOWAY (Tracey); SAKURAI (Tatsuya); ZHIWEI HAN; EHLERS (Susanna); SPAK (Scott N.); HOROWITZ (Larry W.); CARMICHAEL (Gregory R.); STREETS (David G.); HOZUMI (Y.); UEDA (Hiromasa); PARK (S. U.); FUNG (Christopher); KAJINO (M.); THONGBOONCHOO (Narisara); ENGARDT (Magnuz); BENNET (Cecilia); HAYAMI (Hiroshi); SARTELET (Karine); ZIFA WANG; MATSUDA (K.); AMANN (Markus); CARMICHAEL (Gregory R.); UEDA (Hiromasa)</AU>
<AF>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A/Madison, WI 53726/Etats-Unis (1 aut., 4 aut., 5 aut.); Acid Deposition and Oxidant Research Center/Niigata/Japon (2 aut., 3 aut., 9 aut., 10 aut.); Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS)/Chine (3 aut.); NOAA Geophysical Fluid Dynamics Laboratory/Princeton, NJ/Etats-Unis (6 aut.); Center for Global and Regional Environmental Research, University of Iowa/IA/Etats-Unis (7 aut., 14 aut.); Argonne National Laboratory/IL/Etats-Unis (8 aut.); Seoul National University/Seoul/Corée, République de (11 aut.); Hong Kong Environmental Protection Department/Hong-Kong (12 aut.); Disaster Prevention Research Institute, Kyoto University/Kyoto/Japon (13 aut.); Swedish Meteorological and Hydrological Institute/Norrkoping/Suède (15 aut., 16 aut.); Central Research Institute of Electric Power Industry/Chiba/Japon (17 aut.); Centre d'Enseignement et de Recherche en Environnement Atmosphérique/France (18 aut.); Institute of Atmospheric Physics/Beijing/Chine (19 aut.); Meisei University/Tokyo/Japon (20 aut.); International Institute for Applied System Analysis/Laxenburg/Autriche (21 aut.); Department of Chemical and Biochemical Engineering, Center for Global and Regional Environmental Research, University of Iowa/Iowa City, IA 52240/Etats-Unis (1 aut.); Acid Deposition and Oxidant Research Center (ADORC), designated as Network Center for EANET (Acid Deposition Monitoring Network in East Asia)/Japon (2 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2008; Vol. 42; No. 15; Pp. 3543-3561; Bibl. 1 p.3/4</SO>
<LA>Anglais</LA>
<EA>This study quantifies the seasonality and geographic variability of global pollutant inflow to Asia. Asia is often looked to as a major source of intercontinental air pollution transport with rising emissions and efficient pollutant export processes. However, the degree to which foreign emissions have been imported to Asia has not been thoroughly examined. The Model Inter-Comparison Study for Asia (MICS-Asia) is an international collaboration to study air pollution transport and chemistry in Asia. Using the global atmospheric chemistry Model of Ozone and Related Tracers (MOZART v. 2.4), and comparing results with a suite of regional models participating in MICS-Asia, we find that imported O
<sub>3</sub>
contributes significantly throughout Asia. The choice of upper boundary condition is found to be particularly important for O
<sub>3</sub>
, even for surface concentrations. Both North America and Europe contribute to ground-level O
<sub>3</sub>
concentrations throughout the region, though the seasonality of these two sources varies. North American contributions peak at over 10% of monthly mean O
<sub>3</sub>
during winter months in East Asia, compared to Europe's spring- and autumn-maxima (5-8%). In comparison to observed data from the Acid Deposition Monitoring Network in East Asia (EANET), MOZART concentrations for O
<sub>3</sub>
generally fall within the range of the MICS models, but MOZART is unable to capture the fine spatial variability of shorter-lived species as well as the regional models.</EA>
<CC>001D16C03</CC>
<FD>Troposphère; Qualité air; Echelon régional; Relation source puits; Source pollution; Phénomène transport; Transport polluant grande distance; Variation saisonnière; Variation spatiale; Ozone; Polluant secondaire; Composé trace; Monoxyde de carbone; Simulation numérique; Distribution concentration; Etude comparative; Performance algorithme; Prévision pollution atmosphérique; Modèle prévision; Asie</FD>
<ED>Troposphere; Air quality; Regional scope; Source sink relationship; Pollution source; Transport process; Long range pollutant transport; Seasonal variation; Spatial variation; Ozone; Secondary pollutant; Trace compound; Carbon monoxide; Numerical simulation; Concentration distribution; Comparative study; Algorithm performance; Atmospheric pollution forecasting; Forecast model; Asia</ED>
<SD>Troposfera; Calidad aire; Escala regional; Relación fuente sumidero; Fuente polución; Fenómeno transporte; Transporte contaminante gran distancia; Variación estacional; Variación espacial; Ozono; Contaminante secundario; Compuesto huella; Carbono monóxido; Simulación numérica; Distribución concentración; Estudio comparativo; Resultado algoritmo; Previsión contaminación del ambiente; Modelo previsión; Asia</SD>
<LO>INIST-8940B.354000183183120050</LO>
<ID>08-0372728</ID>
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