MICS-Asia II. Impact of global emissions on regional air quality in Asia
Identifieur interne : 000107 ( PascalFrancis/Corpus ); précédent : 000106; suivant : 000108MICS-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 AmannSource :
- Atmospheric environment : (1994) [ 1352-2310 ] ; 2008.
Descripteurs français
- Pascal (Inist)
- 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.
English descriptors
- KwdEn :
- Air quality, Algorithm performance, Asia, Atmospheric pollution forecasting, Carbon monoxide, Comparative study, Concentration distribution, Forecast model, Long range pollutant transport, Numerical simulation, Ozone, Pollution source, Regional scope, Seasonal variation, Secondary pollutant, Source sink relationship, Spatial variation, Trace compound, Transport process, Troposphere.
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.
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Format Inist (serveur)
NO : | PASCAL 08-0372728 INIST |
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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 |
Links to Exploration step
Pascal:08-0372728Le document en format XML
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<sourceDesc><biblStruct><analytic><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>
<affiliation><inist:fA14 i1="01"><s1>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A</s1>
<s2>Madison, WI 53726</s2>
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<author><name sortKey="Sakurai, Tatsuya" sort="Sakurai, Tatsuya" uniqKey="Sakurai T" first="Tatsuya" last="Sakurai">Tatsuya Sakurai</name>
<affiliation><inist:fA14 i1="02"><s1>Acid Deposition and Oxidant Research Center</s1>
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<author><name sortKey="Zhiwei Han" sort="Zhiwei Han" uniqKey="Zhiwei Han" last="Zhiwei Han">ZHIWEI HAN</name>
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<author><name sortKey="Ehlers, Susanna" sort="Ehlers, Susanna" uniqKey="Ehlers S" first="Susanna" last="Ehlers">Susanna Ehlers</name>
<affiliation><inist:fA14 i1="01"><s1>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A</s1>
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<author><name sortKey="Spak, Scott N" sort="Spak, Scott N" uniqKey="Spak S" first="Scott N." last="Spak">Scott N. Spak</name>
<affiliation><inist:fA14 i1="01"><s1>Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Avenue, Room 201A</s1>
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<author><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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<author><name sortKey="Carmichael, Gregory R" sort="Carmichael, Gregory R" uniqKey="Carmichael G" first="Gregory R." last="Carmichael">Gregory R. Carmichael</name>
<affiliation><inist:fA14 i1="05"><s1>Center for Global and Regional Environmental Research, University of Iowa</s1>
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<author><name sortKey="Streets, David G" sort="Streets, David G" uniqKey="Streets D" first="David G." last="Streets">David G. Streets</name>
<affiliation><inist:fA14 i1="06"><s1>Argonne National Laboratory</s1>
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<s3>USA</s3>
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<author><name sortKey="Hozumi, Y" sort="Hozumi, Y" uniqKey="Hozumi Y" first="Y." last="Hozumi">Y. Hozumi</name>
<affiliation><inist:fA14 i1="02"><s1>Acid Deposition and Oxidant Research Center</s1>
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<affiliation><inist:fA14 i1="02"><s1>Acid Deposition and Oxidant Research Center</s1>
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<author><name sortKey="Park, S U" sort="Park, S U" uniqKey="Park S" first="S. U." last="Park">S. U. Park</name>
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<author><name sortKey="Fung, Christopher" sort="Fung, Christopher" uniqKey="Fung C" first="Christopher" last="Fung">Christopher Fung</name>
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<author><name sortKey="Kajino, M" sort="Kajino, M" uniqKey="Kajino M" first="M." last="Kajino">M. Kajino</name>
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<author><name sortKey="Thongboonchoo, Narisara" sort="Thongboonchoo, Narisara" uniqKey="Thongboonchoo N" first="Narisara" last="Thongboonchoo">Narisara Thongboonchoo</name>
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<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>
<sZ>15 aut.</sZ>
<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>
<affiliation><inist:fA14 i1="10"><s1>Swedish Meteorological and Hydrological Institute</s1>
<s2>Norrkoping</s2>
<s3>SWE</s3>
<sZ>15 aut.</sZ>
<sZ>16 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Hayami, Hiroshi" sort="Hayami, Hiroshi" uniqKey="Hayami H" first="Hiroshi" last="Hayami">Hiroshi Hayami</name>
<affiliation><inist:fA14 i1="11"><s1>Central Research Institute of Electric Power Industry</s1>
<s2>Chiba</s2>
<s3>JPN</s3>
<sZ>17 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Sartelet, Karine" sort="Sartelet, Karine" uniqKey="Sartelet K" first="Karine" last="Sartelet">Karine Sartelet</name>
<affiliation><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>
<affiliation><inist:fA14 i1="13"><s1>Institute of Atmospheric Physics</s1>
<s2>Beijing</s2>
<s3>CHN</s3>
<sZ>19 aut.</sZ>
</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>
</analytic>
<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>
</sourceDesc>
<seriesStmt><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>
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<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>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1352-2310</s0>
</fA01>
<fA03 i2="1"><s0>Atmos. environ. : (1994)</s0>
</fA03>
<fA05><s2>42</s2>
</fA05>
<fA06><s2>15</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>MICS-Asia II. Impact of global emissions on regional air quality in Asia</s1>
</fA08>
<fA09 i1="01" i2="1" l="ENG"><s1>MICS-ASIA II</s1>
</fA09>
<fA11 i1="01" i2="1"><s1>HOLLOWAY (Tracey)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>SAKURAI (Tatsuya)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>ZHIWEI HAN</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>EHLERS (Susanna)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>SPAK (Scott N.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>HOROWITZ (Larry W.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>CARMICHAEL (Gregory R.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>STREETS (David G.)</s1>
</fA11>
<fA11 i1="09" i2="1"><s1>HOZUMI (Y.)</s1>
</fA11>
<fA11 i1="10" i2="1"><s1>UEDA (Hiromasa)</s1>
</fA11>
<fA11 i1="11" i2="1"><s1>PARK (S. U.)</s1>
</fA11>
<fA11 i1="12" i2="1"><s1>FUNG (Christopher)</s1>
</fA11>
<fA11 i1="13" i2="1"><s1>KAJINO (M.)</s1>
</fA11>
<fA11 i1="14" i2="1"><s1>THONGBOONCHOO (Narisara)</s1>
</fA11>
<fA11 i1="15" i2="1"><s1>ENGARDT (Magnuz)</s1>
</fA11>
<fA11 i1="16" i2="1"><s1>BENNET (Cecilia)</s1>
</fA11>
<fA11 i1="17" i2="1"><s1>HAYAMI (Hiroshi)</s1>
</fA11>
<fA11 i1="18" i2="1"><s1>SARTELET (Karine)</s1>
</fA11>
<fA11 i1="19" i2="1"><s1>ZIFA WANG</s1>
</fA11>
<fA11 i1="20" i2="1"><s1>MATSUDA (K.)</s1>
</fA11>
<fA11 i1="21" i2="1"><s1>AMANN (Markus)</s1>
</fA11>
<fA12 i1="01" i2="1"><s1>CARMICHAEL (Gregory R.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="02" i2="1"><s1>UEDA (Hiromasa)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><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>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Acid Deposition and Oxidant Research Center</s1>
<s2>Niigata</s2>
<s3>JPN</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>9 aut.</sZ>
<sZ>10 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS)</s1>
<s3>CHN</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>NOAA Geophysical Fluid Dynamics Laboratory</s1>
<s2>Princeton, NJ</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</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>
<s3>USA</s3>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="07"><s1>Seoul National University</s1>
<s2>Seoul</s2>
<s3>KOR</s3>
<sZ>11 aut.</sZ>
</fA14>
<fA14 i1="08"><s1>Hong Kong Environmental Protection Department</s1>
<s3>HKG</s3>
<sZ>12 aut.</sZ>
</fA14>
<fA14 i1="09"><s1>Disaster Prevention Research Institute, Kyoto University</s1>
<s2>Kyoto</s2>
<s3>JPN</s3>
<sZ>13 aut.</sZ>
</fA14>
<fA14 i1="10"><s1>Swedish Meteorological and Hydrological Institute</s1>
<s2>Norrkoping</s2>
<s3>SWE</s3>
<sZ>15 aut.</sZ>
<sZ>16 aut.</sZ>
</fA14>
<fA14 i1="11"><s1>Central Research Institute of Electric Power Industry</s1>
<s2>Chiba</s2>
<s3>JPN</s3>
<sZ>17 aut.</sZ>
</fA14>
<fA14 i1="12"><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>
</fA15>
<fA20><s1>3543-3561</s1>
</fA20>
<fA21><s1>2008</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>8940B</s2>
<s5>354000183183120050</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2008 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.3/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>08-0372728</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<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>
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<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>
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<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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