MozartV1, PascalFrancis, Corpus, bibRecord, 000137

Satellite measurements of tropospheric column O3 and NO2 in eastern and southeastern Asia : Comparison with a global model (MOZART-2)

Identifieur interne : 000137 ( PascalFrancis/Corpus ); précédent : 000136; suivant : 000138

Satellite measurements of tropospheric column O3 and NO2 in eastern and southeastern Asia : Comparison with a global model (MOZART-2)

Auteurs : X. Tie ; S. Chandra ; J. R. Ziemke ; C. Granier ; G. P. Brasseur

Source :

Journal of atmospheric chemistry [ 0167-7764 ] ; 2007.

RBID : Pascal:07-0153872

Descripteurs français

Pascal (Inist)
- Troposphère, Pollution air, Oxydant photochimique, Ozone, Azote dioxyde, Distribution concentration, Profil vertical, Répartition spatiale, Variation saisonnière, Donnée observation, Observation par satellite, Satellite UARS, Source pollution, Facteur anthropique, Analyse sensibilité, Asie, Télédétection spatiale.

English descriptors

KwdEn :
- Air pollution, Anthropogenic factor, Asia, Concentration distribution, Nitrogen dioxide, Observation data, Ozone, Photochemical oxidants, Pollution source, Satellite observation, Seasonal variation, Sensitivity analysis, Space remote sensing, Spatial distribution, Troposphere, UARS satellite, Vertical profile.

Abstract

Satellite measurements of tropospheric column O₃ and NO₂ in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O₃ is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO₂ is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O₃ and NO₂ fields. The analysis of the model results show that the industrial emission of NO_x (TMO+NO₂) contributes about 50%-80% to tropospheric column NO₂ in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O₃ ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO_x emissions have a small effect on tropospheric O₃ in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO_x on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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C01	`01`		`ENG`	@0 Satellite measurements of tropospheric column O₃ and NO₂ in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O₃ is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO₂ is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O₃ and NO₂ fields. The analysis of the model results show that the industrial emission of NO_x (TMO+NO₂) contributes about 50%-80% to tropospheric column NO₂ in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O₃ ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO_x emissions have a small effect on tropospheric O₃ in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO_x on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.
C02	`01`	`X`		`@0 001D16C02`
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Format Inist (serveur)

NO :	PASCAL 07-0153872 INIST
ET :	Satellite measurements of tropospheric column O₃ and NO₂ in eastern and southeastern Asia : Comparison with a global model (MOZART-2)
AU :	TIE (X.); CHANDRA (S.); ZIEMKE (J. R.); GRANIER (C.); BRASSEUR (G. P.)
AF :	National Center of Atmospheric Research/Boulder, CO/Etats-Unis (1 aut., 5 aut.); University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)/Baltimore, MD/Etats-Unis (2 aut., 3 aut.); NASA Goddard Space Flight Center, Code 613.3/Greenbelt, MD/Etats-Unis (2 aut., 3 aut.); NOAA/Boulder, CO/Etats-Unis (4 aut.); Max Planck Institute of Meteorology/Hamburg/Allemagne (5 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of atmospheric chemistry; ISSN 0167-7764; Coden JATCE2; Pays-Bas; Da. 2007; Vol. 56; No. 2; Pp. 105-125; Bibl. 1 p.1/4
LA :	Anglais
EA :	Satellite measurements of tropospheric column O₃ and NO₂ in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O₃ is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO₂ is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O₃ and NO₂ fields. The analysis of the model results show that the industrial emission of NO_x (TMO+NO₂) contributes about 50%-80% to tropospheric column NO₂ in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O₃ ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO_x emissions have a small effect on tropospheric O₃ in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO_x on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.
CC :	001D16C02
FD :	Troposphère; Pollution air; Oxydant photochimique; Ozone; Azote dioxyde; Distribution concentration; Profil vertical; Répartition spatiale; Variation saisonnière; Donnée observation; Observation par satellite; Satellite UARS; Source pollution; Facteur anthropique; Analyse sensibilité; Asie; Télédétection spatiale
ED :	Troposphere; Air pollution; Photochemical oxidants; Ozone; Nitrogen dioxide; Concentration distribution; Vertical profile; Spatial distribution; Seasonal variation; Observation data; Satellite observation; UARS satellite; Pollution source; Anthropogenic factor; Sensitivity analysis; Asia; Space remote sensing
SD :	Troposfera; Contaminación aire; Ozono; Nitrógeno dióxido; Distribución concentración; Perfil vertical; Distribución espacial; Variación estacional; Dato observación; Observación por satélite; Satélite UARS; Fuente polución; Factor antrópico; Análisis sensibilidad; Asia; Teledetección espacial
LO :	INIST-19998.354000146888900010
ID :	07-0153872

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Pascal:07-0153872

Le document en format XML

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<term>Ozone</term>
<term>Photochemical oxidants</term>
<term>Pollution source</term>
<term>Satellite observation</term>
<term>Seasonal variation</term>
<term>Sensitivity analysis</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Troposphère</term>
<term>Pollution air</term>
<term>Oxydant photochimique</term>
<term>Ozone</term>
<term>Azote dioxyde</term>
<term>Distribution concentration</term>
<term>Profil vertical</term>
<term>Répartition spatiale</term>
<term>Variation saisonnière</term>
<term>Donnée observation</term>
<term>Observation par satellite</term>
<term>Satellite UARS</term>
<term>Source pollution</term>
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<front><div type="abstract" xml:lang="en">Satellite measurements of tropospheric column O<sub>3</sub>
 and NO<sub>2</sub>
 in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O<sub>3</sub>
 is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO<sub>2</sub>
 is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O<sub>3</sub>
 and NO<sub>2</sub>
 fields. The analysis of the model results show that the industrial emission of NO<sub>x</sub>
 (TMO+NO<sub>2</sub>
) contributes about 50%-80% to tropospheric column NO<sub>2</sub>
 in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O<sub>3</sub>
 ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO<sub>x</sub>
 emissions have a small effect on tropospheric O<sub>3</sub>
 in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO<sub>x</sub>
 on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.</div>
</front>
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<fA11 i1="03" i2="1"><s1>ZIEMKE (J. R.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>GRANIER (C.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>BRASSEUR (G. P.)</s1>
</fA11>
<fA14 i1="01"><s1>National Center of Atmospheric Research</s1>
<s2>Boulder, CO</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)</s1>
<s2>Baltimore, MD</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>NASA Goddard Space Flight Center, Code 613.3</s1>
<s2>Greenbelt, MD</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>NOAA</s1>
<s2>Boulder, CO</s2>
<s3>USA</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Max Planck Institute of Meteorology</s1>
<s2>Hamburg</s2>
<s3>DEU</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA20><s1>105-125</s1>
</fA20>
<fA21><s1>2007</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>19998</s2>
<s5>354000146888900010</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2007 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>07-0153872</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of atmospheric chemistry</s0>
</fA64>
<fA66 i1="01"><s0>NLD</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Satellite measurements of tropospheric column O<sub>3</sub>
 and NO<sub>2</sub>
 in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O<sub>3</sub>
 is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO<sub>2</sub>
 is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O<sub>3</sub>
 and NO<sub>2</sub>
 fields. The analysis of the model results show that the industrial emission of NO<sub>x</sub>
 (TMO+NO<sub>2</sub>
) contributes about 50%-80% to tropospheric column NO<sub>2</sub>
 in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O<sub>3</sub>
 ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO<sub>x</sub>
 emissions have a small effect on tropospheric O<sub>3</sub>
 in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO<sub>x</sub>
 on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001D16C02</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>Pollution air</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Air pollution</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Contaminación aire</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="3" l="FRE"><s0>Oxydant photochimique</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="3" l="ENG"><s0>Photochemical oxidants</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Ozono</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Azote dioxyde</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Nitrogen dioxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Nitrógeno dióxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Distribution concentration</s0>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Concentration distribution</s0>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Distribución concentración</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Profil vertical</s0>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Vertical profile</s0>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Perfil vertical</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Répartition spatiale</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Spatial distribution</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Distribución espacial</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Variation saisonnière</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Seasonal variation</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Variación estacional</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Donnée observation</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Observation data</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Dato observación</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Observation par satellite</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Satellite observation</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Observación por satélite</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Satellite UARS</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>UARS satellite</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Satélite UARS</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Source pollution</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Pollution source</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Fuente polución</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Facteur anthropique</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Anthropogenic factor</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Factor antrópico</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Analyse sensibilité</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Sensitivity analysis</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Análisis sensibilidad</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="X" l="FRE"><s0>Asie</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="16" i2="X" l="ENG"><s0>Asia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="16" i2="X" l="SPA"><s0>Asia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE"><s0>Télédétection spatiale</s0>
<s5>31</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG"><s0>Space remote sensing</s0>
<s5>31</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA"><s0>Teledetección espacial</s0>
<s5>31</s5>
</fC03>
<fN21><s1>099</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 07-0153872 INIST</NO>
<ET>Satellite measurements of tropospheric column O<sub>3</sub>
 and NO<sub>2</sub>
 in eastern and southeastern Asia : Comparison with a global model (MOZART-2)</ET>
<AU>TIE (X.); CHANDRA (S.); ZIEMKE (J. R.); GRANIER (C.); BRASSEUR (G. P.)</AU>
<AF>National Center of Atmospheric Research/Boulder, CO/Etats-Unis (1 aut., 5 aut.); University of Maryland Baltimore County (UMBC) Goddard Earth Sciences and Technology (GEST)/Baltimore, MD/Etats-Unis (2 aut., 3 aut.); NASA Goddard Space Flight Center, Code 613.3/Greenbelt, MD/Etats-Unis (2 aut., 3 aut.); NOAA/Boulder, CO/Etats-Unis (4 aut.); Max Planck Institute of Meteorology/Hamburg/Allemagne (5 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of atmospheric chemistry; ISSN 0167-7764; Coden JATCE2; Pays-Bas; Da. 2007; Vol. 56; No. 2; Pp. 105-125; Bibl. 1 p.1/4</SO>
<LA>Anglais</LA>
<EA>Satellite measurements of tropospheric column O<sub>3</sub>
 and NO<sub>2</sub>
 in eastern and southeastern Asia are analyzed to study the spatial and seasonal characteristics of pollution in these regions. Tropospheric column O<sub>3</sub>
 is derived from differential measurements of total column ozone from Total Ozone Mapping Spectrometer (TOMS), and stratospheric column ozone from the Microwave Limb Sounder (MLS) instrument on the Upper Atmosphere Research Satellite (UARS). The tropospheric column NO<sub>2</sub>
 is measured by Global Ozone Monitoring Experiment (GOME). A global chemical and transport model (Model of Ozone and Related Chemical Tracers, version 2; MOZART-2) is applied to analyze and interpret the satellite measurements. The study, which is based on spring, summer, and fall months of 1997 shows generally good agreement between the model and satellite data with respect to seasonal and spatial characteristics of O<sub>3</sub>
 and NO<sub>2</sub>
 fields. The analysis of the model results show that the industrial emission of NO<sub>x</sub>
 (TMO+NO<sub>2</sub>
) contributes about 50%-80% to tropospheric column NO<sub>2</sub>
 in eastern Asia and about 20%-50% in southeastern Asia. The contribution of industrial emission of NO, to tropospheric column O<sub>3</sub>
 ranges from 10% to 30% in eastern Asia. Biomass burning and lightning NO<sub>x</sub>
 emissions have a small effect on tropospheric O<sub>3</sub>
 in central and eastern Asia, but they have a significant impact in southeastern Asia. The varying effects of NO<sub>x</sub>
 on tropospheric column ozone are attributed to differences in relative abundance of volatile organic compounds (VOCs) with respect to total nitrogen in the two regions.</EA>
<CC>001D16C02</CC>
<FD>Troposphère; Pollution air; Oxydant photochimique; Ozone; Azote dioxyde; Distribution concentration; Profil vertical; Répartition spatiale; Variation saisonnière; Donnée observation; Observation par satellite; Satellite UARS; Source pollution; Facteur anthropique; Analyse sensibilité; Asie; Télédétection spatiale</FD>
<ED>Troposphere; Air pollution; Photochemical oxidants; Ozone; Nitrogen dioxide; Concentration distribution; Vertical profile; Spatial distribution; Seasonal variation; Observation data; Satellite observation; UARS satellite; Pollution source; Anthropogenic factor; Sensitivity analysis; Asia; Space remote sensing</ED>
<SD>Troposfera; Contaminación aire; Ozono; Nitrógeno dióxido; Distribución concentración; Perfil vertical; Distribución espacial; Variación estacional; Dato observación; Observación por satélite; Satélite UARS; Fuente polución; Factor antrópico; Análisis sensibilidad; Asia; Teledetección espacial</SD>
<LO>INIST-19998.354000146888900010</LO>
<ID>07-0153872</ID>
</server>
</inist>
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Satellite measurements of tropospheric column O3 and NO2 in eastern and southeastern Asia : Comparison with a global model (MOZART-2)

Satellite measurements of tropospheric column O3 and NO2 in eastern and southeastern Asia : Comparison with a global model (MOZART-2)

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