MozartV1, PascalFrancis, Corpus, bibRecord, 000002

Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region

Identifieur interne : 000002 ( PascalFrancis/Corpus ); précédent : 000001; suivant : 000003

Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region

Auteurs : XUEWEI HOU ; BIN ZHU ; HANQING KANG ; JINHUI GAO

Source :

Atmospheric environment : (1994) [ 1352-2310 ] ; 2014.

RBID : Pascal:14-0262769

Descripteurs français

Pascal (Inist)
- Ozone, Couche limite atmosphérique, Variation saisonnière, Bilan matière, Gradient latitudinal, Variation spatiale, Pollution air, Source pollution, Asie, Océan Pacifique, Oxydant photochimique.

English descriptors

KwdEn :
- Air pollution, Asia, Atmospheric boundary layer, Latitudinal gradient, Material balance, Ozone, Pacific Ocean, Photochemical oxidants, Pollution source, Seasonal variation, Spatial variation.

Abstract

The ozone (O₃) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O₃ data agree well with observed values. O₃ budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O₃ differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O₃ concentrations. The large latitudinal gradient in O₃ with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O₃ was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O₃ export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 1352-2310`
A03		`1`		`@0 Atmos. environ. : (1994)`
A05				`@2 94`
A08	`01`	`1`	`ENG`	`@1 Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region`
A11	`01`	`1`		`@1 XUEWEI HOU`
A11	`02`	`1`		`@1 BIN ZHU`
A11	`03`	`1`		`@1 HANQING KANG`
A11	`04`	`1`		`@1 JINHUI GAO`
A14	`01`			`@1 Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology @2 Nanjing 210044 @3 CHN @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut.`
A14	`02`			`@1 Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science & Technology @2 Nanjing 210044 @3 CHN @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut.`
A20				`@1 734-741`
A21				`@1 2014`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 8940B @5 354000150337810780`
A44				`@0 0000 @1 © 2014 INIST-CNRS. All rights reserved.`
A45				`@0 1 p.`
A47	`01`	`1`		`@0 14-0262769`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Atmospheric environment : (1994)`
A66	`01`			`@0 GBR`
C01	`01`		`ENG`	@0 The ozone (O₃) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O₃ data agree well with observed values. O₃ budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O₃ differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O₃ concentrations. The large latitudinal gradient in O₃ with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O₃ was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O₃ export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.
C02	`01`	`X`		`@0 001D16C02`
C03	`01`	`X`	`FRE`	`@0 Ozone @2 NK @2 FX @5 01`
C03	`01`	`X`	`ENG`	`@0 Ozone @2 NK @2 FX @5 01`
C03	`01`	`X`	`SPA`	`@0 Ozono @2 NK @2 FX @5 01`
C03	`02`	`X`	`FRE`	`@0 Couche limite atmosphérique @5 02`
C03	`02`	`X`	`ENG`	`@0 Atmospheric boundary layer @5 02`
C03	`02`	`X`	`SPA`	`@0 Capa límite atmosférico @5 02`
C03	`03`	`X`	`FRE`	`@0 Variation saisonnière @5 03`
C03	`03`	`X`	`ENG`	`@0 Seasonal variation @5 03`
C03	`03`	`X`	`SPA`	`@0 Variación estacional @5 03`
C03	`04`	`X`	`FRE`	`@0 Bilan matière @5 04`
C03	`04`	`X`	`ENG`	`@0 Material balance @5 04`
C03	`04`	`X`	`SPA`	`@0 Balance materia @5 04`
C03	`05`	`X`	`FRE`	`@0 Gradient latitudinal @5 05`
C03	`05`	`X`	`ENG`	`@0 Latitudinal gradient @5 05`
C03	`05`	`X`	`SPA`	`@0 Gradiente latitudinal @5 05`
C03	`06`	`X`	`FRE`	`@0 Variation spatiale @5 06`
C03	`06`	`X`	`ENG`	`@0 Spatial variation @5 06`
C03	`06`	`X`	`SPA`	`@0 Variación espacial @5 06`
C03	`07`	`X`	`FRE`	`@0 Pollution air @5 07`
C03	`07`	`X`	`ENG`	`@0 Air pollution @5 07`
C03	`07`	`X`	`SPA`	`@0 Contaminación aire @5 07`
C03	`08`	`X`	`FRE`	`@0 Source pollution @5 08`
C03	`08`	`X`	`ENG`	`@0 Pollution source @5 08`
C03	`08`	`X`	`SPA`	`@0 Fuente polución @5 08`
C03	`09`	`X`	`FRE`	`@0 Asie @2 NG @5 31`
C03	`09`	`X`	`ENG`	`@0 Asia @2 NG @5 31`
C03	`09`	`X`	`SPA`	`@0 Asia @2 NG @5 31`
C03	`10`	`X`	`FRE`	`@0 Océan Pacifique @2 NG @5 32`
C03	`10`	`X`	`ENG`	`@0 Pacific Ocean @2 NG @5 32`
C03	`10`	`X`	`SPA`	`@0 Océano Pacífico @2 NG @5 32`
C03	`11`	`3`	`FRE`	`@0 Oxydant photochimique @5 35`
C03	`11`	`3`	`ENG`	`@0 Photochemical oxidants @5 35`
N21				`@1 328`

Format Inist (serveur)

NO :	PASCAL 14-0262769 INIST
ET :	Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region
AU :	XUEWEI HOU; BIN ZHU; HANQING KANG; JINHUI GAO
AF :	Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology/Nanjing 210044/Chine (1 aut., 2 aut., 3 aut., 4 aut.); Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science & Technology/Nanjing 210044/Chine (1 aut., 2 aut., 3 aut., 4 aut.)
DT :	Publication en série; Niveau analytique
SO :	Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2014; Vol. 94; Pp. 734-741; Bibl. 1 p.
LA :	Anglais
EA :	The ozone (O₃) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O₃ data agree well with observed values. O₃ budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O₃ differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O₃ concentrations. The large latitudinal gradient in O₃ with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O₃ was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O₃ export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.
CC :	001D16C02
FD :	Ozone; Couche limite atmosphérique; Variation saisonnière; Bilan matière; Gradient latitudinal; Variation spatiale; Pollution air; Source pollution; Asie; Océan Pacifique; Oxydant photochimique
ED :	Ozone; Atmospheric boundary layer; Seasonal variation; Material balance; Latitudinal gradient; Spatial variation; Air pollution; Pollution source; Asia; Pacific Ocean; Photochemical oxidants
SD :	Ozono; Capa límite atmosférico; Variación estacional; Balance materia; Gradiente latitudinal; Variación espacial; Contaminación aire; Fuente polución; Asia; Océano Pacífico
LO :	INIST-8940B.354000150337810780
ID :	14-0262769

Links to Exploration step

Pascal:14-0262769

Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Air pollution</term>
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<front><div type="abstract" xml:lang="en">The ozone (O<sub>3</sub>
) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O<sub>3</sub>
 data agree well with observed values. O<sub>3</sub>
 budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O<sub>3</sub>
 differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O<sub>3</sub>
 concentrations. The large latitudinal gradient in O<sub>3</sub>
 with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O<sub>3</sub>
 was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O<sub>3</sub>
 export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.</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>94</s2>
</fA05>
<fA08 i1="01" i2="1" l="ENG"><s1>Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>XUEWEI HOU</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>BIN ZHU</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>HANQING KANG</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>JINHUI GAO</s1>
</fA11>
<fA14 i1="01"><s1>Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology</s1>
<s2>Nanjing 210044</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science & Technology</s1>
<s2>Nanjing 210044</s2>
<s3>CHN</s3>
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<fA66 i1="01"><s0>GBR</s0>
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<fC01 i1="01" l="ENG"><s0>The ozone (O<sub>3</sub>
) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O<sub>3</sub>
 data agree well with observed values. O<sub>3</sub>
 budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O<sub>3</sub>
 differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O<sub>3</sub>
 concentrations. The large latitudinal gradient in O<sub>3</sub>
 with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O<sub>3</sub>
 was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O<sub>3</sub>
 export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001D16C02</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Ozono</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Couche limite atmosphérique</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Atmospheric boundary layer</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Capa límite atmosférico</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Variation saisonnière</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Seasonal variation</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Variación estacional</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Bilan matière</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Material balance</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Balance materia</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Gradient latitudinal</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Latitudinal gradient</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Gradiente latitudinal</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Variation spatiale</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Spatial variation</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Variación espacial</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Pollution air</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Air pollution</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Contaminación aire</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Source pollution</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Pollution source</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Fuente polución</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Asie</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Asia</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Asia</s0>
<s2>NG</s2>
<s5>31</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Océan Pacifique</s0>
<s2>NG</s2>
<s5>32</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Pacific Ocean</s0>
<s2>NG</s2>
<s5>32</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Océano Pacífico</s0>
<s2>NG</s2>
<s5>32</s5>
</fC03>
<fC03 i1="11" i2="3" l="FRE"><s0>Oxydant photochimique</s0>
<s5>35</s5>
</fC03>
<fC03 i1="11" i2="3" l="ENG"><s0>Photochemical oxidants</s0>
<s5>35</s5>
</fC03>
<fN21><s1>328</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 14-0262769 INIST</NO>
<ET>Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region</ET>
<AU>XUEWEI HOU; BIN ZHU; HANQING KANG; JINHUI GAO</AU>
<AF>Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology/Nanjing 210044/Chine (1 aut., 2 aut., 3 aut., 4 aut.); Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science & Technology/Nanjing 210044/Chine (1 aut., 2 aut., 3 aut., 4 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2014; Vol. 94; Pp. 734-741; Bibl. 1 p.</SO>
<LA>Anglais</LA>
<EA>The ozone (O<sub>3</sub>
) budget in the boundary layer of the Asia-Pacific region (AP) was studied from 2001 to 2007 using the output of Model of Ozone and Related chemical Tracers, version 4 (MOZART-4). The model-simulated O<sub>3</sub>
 data agree well with observed values. O<sub>3</sub>
 budget analysis using the model output confirms that the dominant factor controlling seasonal variation of O<sub>3</sub>
 differs by region. Photochemistry was found to play a critical role over Japan, the Korean Peninsula and Eastern China. Over the north-western Pacific Ocean, advective flux was found to drive the seasonal variation of O<sub>3</sub>
 concentrations. The large latitudinal gradient in O<sub>3</sub>
 with a maximum of 52 ppbv over the marine boundary layer around 35°N during the spring was mainly due to chemistry; meanwhile, advection was found to weaken the gradient. The contribution of stratospheric O<sub>3</sub>
 was ranked second (20%) to the local contribution (25%) in Japan and the Korean Peninsula near 35°N. The rate of O<sub>3</sub>
 export from China's boundary layer was the highest (approximately 30%) in low latitudes and decreased with increasing latitude, while the contribution of North America and Europe increased with increasing latitude, from 10% in lower latitudes to 24% in higher latitudes.</EA>
<CC>001D16C02</CC>
<FD>Ozone; Couche limite atmosphérique; Variation saisonnière; Bilan matière; Gradient latitudinal; Variation spatiale; Pollution air; Source pollution; Asie; Océan Pacifique; Oxydant photochimique</FD>
<ED>Ozone; Atmospheric boundary layer; Seasonal variation; Material balance; Latitudinal gradient; Spatial variation; Air pollution; Pollution source; Asia; Pacific Ocean; Photochemical oxidants</ED>
<SD>Ozono; Capa límite atmosférico; Variación estacional; Balance materia; Gradiente latitudinal; Variación espacial; Contaminación aire; Fuente polución; Asia; Océano Pacífico</SD>
<LO>INIST-8940B.354000150337810780</LO>
<ID>14-0262769</ID>
</server>
</inist>
</record>

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Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region

Analysis of seasonal ozone budget and spring ozone latitudinal gradient variation in the boundary layer of the Asia-Pacific region

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