MozartV1, PascalFrancis, Corpus, bibRecord, 000218

Model derived tropospheric NO2 columns compared with GOME measurements

Identifieur interne : 000218 ( PascalFrancis/Corpus ); précédent : 000217; suivant : 000219

Model derived tropospheric NO2 columns compared with GOME measurements

Auteurs : G. J. M. Velders ; C. Granier ; R. W. Portmann ; K. Pfeilsticker ; M. Wenig ; T. Wagner ; C. Leue ; U. Platt ; A. Richter ; J. P. Burrows

Source :

RBID : Pascal:02-0074706

Descripteurs français

Pascal (Inist)
- Troposphère, Pollution air, Qualité air, Azote dioxyde, Teneur, Variation temporelle, Variation spatiale, Surveillance, Télédétection, Observation par satellite, Modélisation.

English descriptors

KwdEn :
- Air pollution, Air quality, Content, Modeling, Nitrogen dioxide, Remote sensing, Satellite observation, Spatial variation, Surveillance, Time variation, Troposphere.

Abstract

Tropospheric NO₂ columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO₂. The measured and modelled NO₂ columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO₂ columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO₂ columns as well as the columns measured by GOME are in good agreement with NO₂ columns derived from observed NO₂ mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO₂ columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A08	`01`	`1`	`ENG`	`@1 Model derived tropospheric NO₂ columns compared with GOME measurements`
A09	`01`	`1`	`ENG`	`@1 Air pollution VIII : Cambridge, 2000`
A11	`01`	`1`		`@1 VELDERS (G. J. M.)`
A11	`02`	`1`		`@1 GRANIER (C.)`
A11	`03`	`1`		`@1 PORTMANN (R. W.)`
A11	`04`	`1`		`@1 PFEILSTICKER (K.)`
A11	`05`	`1`		`@1 WENIG (M.)`
A11	`06`	`1`		`@1 WAGNER (T.)`
A11	`07`	`1`		`@1 LEUE (C.)`
A11	`08`	`1`		`@1 PLATT (U.)`
A11	`09`	`1`		`@1 RICHTER (A.)`
A11	`10`	`1`		`@1 BURROWS (J. P.)`
A12	`01`	`1`		`@1 LONGHURST (J.W.S.) @9 ed.`
A12	`02`	`1`		`@1 BREBBIA (C.A.) @9 ed.`
A12	`03`	`1`		`@1 POWER (H.) @9 ed.`
A14	`01`			`@1 Air Research Laboratory, National Institute of Public Health and the Environment @2 Bilthoven @3 NLD @Z 1 aut.`
A14	`02`			`@1 Aeronomy Laboratory, NOAA @2 Boulder @3 USA @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut.`
A14	`03`			`@1 Service d'Aéronomie CNRS @2 Paris @3 FRA @Z 2 aut.`
A14	`04`			`@1 CIRES, University of Colorado @2 Boulder @3 USA @Z 2 aut.`
A14	`05`			`@1 Institut für Umweltphysik, University of Heidelberg @3 DEU @Z 4 aut. @Z 5 aut. @Z 6 aut. @Z 7 aut. @Z 8 aut.`
A14	`06`			`@1 Institute of Environmental Physics, University of Bremen @3 DEU @Z 9 aut. @Z 10 aut.`
A20				`@1 463-472`
A21				`@1 2000`
A23	`01`			`@0 ENG`
A25	`01`			`@1 WIT Press @2 Southampton`
A26	`01`			`@0 1-85312-822-8`
A30	`01`	`1`	`ENG`	`@1 International conference on air pollution @2 8 @3 Cambridge GBR @4 2000`
A43	`01`			`@1 INIST @2 Y 33598 @5 354000097037380470`
A44				`@0 0000 @1 © 2002 INIST-CNRS. All rights reserved.`
A45				`@0 11 ref.`
A47	`01`	`1`		`@0 02-0074706`
A60				`@1 C`
A61				`@0 A`
A66	`01`			`@0 GBR`
C01	`01`		`ENG`	@0 Tropospheric NO₂ columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO₂. The measured and modelled NO₂ columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO₂ columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO₂ columns as well as the columns measured by GOME are in good agreement with NO₂ columns derived from observed NO₂ mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO₂ columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.
C02	`01`	`X`		`@0 001D16C02`
C02	`02`	`X`		`@0 001E02D04`
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 Pollution air @5 08`
C03	`02`	`X`	`ENG`	`@0 Air pollution @5 08`
C03	`02`	`X`	`SPA`	`@0 Contaminación aire @5 08`
C03	`03`	`X`	`FRE`	`@0 Qualité air @5 09`
C03	`03`	`X`	`ENG`	`@0 Air quality @5 09`
C03	`03`	`X`	`SPA`	`@0 Calidad aire @5 09`
C03	`04`	`X`	`FRE`	`@0 Azote dioxyde @2 NK @2 FX @5 11`
C03	`04`	`X`	`ENG`	`@0 Nitrogen dioxide @2 NK @2 FX @5 11`
C03	`04`	`X`	`SPA`	`@0 Nitrógeno dióxido @2 NK @2 FX @5 11`
C03	`05`	`X`	`FRE`	`@0 Teneur @5 12`
C03	`05`	`X`	`ENG`	`@0 Content @5 12`
C03	`05`	`X`	`SPA`	`@0 Proporción @5 12`
C03	`06`	`X`	`FRE`	`@0 Variation temporelle @5 13`
C03	`06`	`X`	`ENG`	`@0 Time variation @5 13`
C03	`06`	`X`	`SPA`	`@0 Variación temporal @5 13`
C03	`07`	`X`	`FRE`	`@0 Variation spatiale @5 14`
C03	`07`	`X`	`ENG`	`@0 Spatial variation @5 14`
C03	`07`	`X`	`SPA`	`@0 Variación espacial @5 14`
C03	`08`	`X`	`FRE`	`@0 Surveillance @5 15`
C03	`08`	`X`	`ENG`	`@0 Surveillance @5 15`
C03	`08`	`X`	`SPA`	`@0 Vigilancia @5 15`
C03	`09`	`X`	`FRE`	`@0 Télédétection @5 16`
C03	`09`	`X`	`ENG`	`@0 Remote sensing @5 16`
C03	`09`	`X`	`SPA`	`@0 Teledetección @5 16`
C03	`10`	`X`	`FRE`	`@0 Observation par satellite @5 17`
C03	`10`	`X`	`ENG`	`@0 Satellite observation @5 17`
C03	`10`	`X`	`SPA`	`@0 Observación por satélite @5 17`
C03	`11`	`X`	`FRE`	`@0 Modélisation @5 18`
C03	`11`	`X`	`ENG`	`@0 Modeling @5 18`
C03	`11`	`X`	`SPA`	`@0 Modelización @5 18`
N21				`@1 037`

Format Inist (serveur)

NO :	PASCAL 02-0074706 INIST
ET :	Model derived tropospheric NO₂ columns compared with GOME measurements
AU :	VELDERS (G. J. M.); GRANIER (C.); PORTMANN (R. W.); PFEILSTICKER (K.); WENIG (M.); WAGNER (T.); LEUE (C.); PLATT (U.); RICHTER (A.); BURROWS (J. P.); LONGHURST (J.W.S.); BREBBIA (C.A.); POWER (H.)
AF :	Air Research Laboratory, National Institute of Public Health and the Environment/Bilthoven/Pays-Bas (1 aut.); Aeronomy Laboratory, NOAA/Boulder/Etats-Unis (1 aut., 2 aut., 3 aut., 4 aut.); Service d'Aéronomie CNRS/Paris/France (2 aut.); CIRES, University of Colorado/Boulder/Etats-Unis (2 aut.); Institut für Umweltphysik, University of Heidelberg/Allemagne (4 aut., 5 aut., 6 aut., 7 aut., 8 aut.); Institute of Environmental Physics, University of Bremen/Allemagne (9 aut., 10 aut.)
DT :	Congrès; Niveau analytique
SO :	International conference on air pollution/8/2000/Cambridge GBR; Royaume-Uni; Southampton: WIT Press; Da. 2000; Pp. 463-472; ISBN 1-85312-822-8
LA :	Anglais
EA :	Tropospheric NO₂ columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO₂. The measured and modelled NO₂ columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO₂ columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO₂ columns as well as the columns measured by GOME are in good agreement with NO₂ columns derived from observed NO₂ mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO₂ columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.
CC :	001D16C02; 001E02D04
FD :	Troposphère; Pollution air; Qualité air; Azote dioxyde; Teneur; Variation temporelle; Variation spatiale; Surveillance; Télédétection; Observation par satellite; Modélisation
ED :	Troposphere; Air pollution; Air quality; Nitrogen dioxide; Content; Time variation; Spatial variation; Surveillance; Remote sensing; Satellite observation; Modeling
SD :	Troposfera; Contaminación aire; Calidad aire; Nitrógeno dióxido; Proporción; Variación temporal; Variación espacial; Vigilancia; Teledetección; Observación por satélite; Modelización
LO :	INIST-Y 33598.354000097037380470
ID :	02-0074706

Links to Exploration step

Pascal:02-0074706

Le document en format XML

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<author><name sortKey="Wenig, M" sort="Wenig, M" uniqKey="Wenig M" first="M." last="Wenig">M. Wenig</name>
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<author><name sortKey="Wagner, T" sort="Wagner, T" uniqKey="Wagner T" first="T." last="Wagner">T. Wagner</name>
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<author><name sortKey="Leue, C" sort="Leue, C" uniqKey="Leue C" first="C." last="Leue">C. Leue</name>
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<author><name sortKey="Platt, U" sort="Platt, U" uniqKey="Platt U" first="U." last="Platt">U. Platt</name>
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<author><name sortKey="Richter, A" sort="Richter, A" uniqKey="Richter A" first="A." last="Richter">A. Richter</name>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Air pollution</term>
<term>Air quality</term>
<term>Content</term>
<term>Modeling</term>
<term>Nitrogen dioxide</term>
<term>Remote sensing</term>
<term>Satellite observation</term>
<term>Spatial variation</term>
<term>Surveillance</term>
<term>Time variation</term>
<term>Troposphere</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Troposphère</term>
<term>Pollution air</term>
<term>Qualité air</term>
<term>Azote dioxyde</term>
<term>Teneur</term>
<term>Variation temporelle</term>
<term>Variation spatiale</term>
<term>Surveillance</term>
<term>Télédétection</term>
<term>Observation par satellite</term>
<term>Modélisation</term>
</keywords>
</textClass>
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<front><div type="abstract" xml:lang="en">Tropospheric NO<sub>2</sub>
 columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO<sub>2</sub>
. The measured and modelled NO<sub>2</sub>
 columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO<sub>2</sub>
 columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO<sub>2</sub>
 columns as well as the columns measured by GOME are in good agreement with NO<sub>2</sub>
 columns derived from observed NO<sub>2</sub>
 mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO<sub>2</sub>
 columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA08 i1="01" i2="1" l="ENG"><s1>Model derived tropospheric NO<sub>2</sub>
 columns compared with GOME measurements</s1>
</fA08>
<fA09 i1="01" i2="1" l="ENG"><s1>Air pollution VIII : Cambridge, 2000</s1>
</fA09>
<fA11 i1="01" i2="1"><s1>VELDERS (G. J. M.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>GRANIER (C.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>PORTMANN (R. W.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>PFEILSTICKER (K.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>WENIG (M.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>WAGNER (T.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>LEUE (C.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>PLATT (U.)</s1>
</fA11>
<fA11 i1="09" i2="1"><s1>RICHTER (A.)</s1>
</fA11>
<fA11 i1="10" i2="1"><s1>BURROWS (J. P.)</s1>
</fA11>
<fA12 i1="01" i2="1"><s1>LONGHURST (J.W.S.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="02" i2="1"><s1>BREBBIA (C.A.)</s1>
<s9>ed.</s9>
</fA12>
<fA12 i1="03" i2="1"><s1>POWER (H.)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><s1>Air Research Laboratory, National Institute of Public Health and the Environment</s1>
<s2>Bilthoven</s2>
<s3>NLD</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Aeronomy Laboratory, NOAA</s1>
<s2>Boulder</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Service d'Aéronomie CNRS</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>CIRES, University of Colorado</s1>
<s2>Boulder</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Institut für Umweltphysik, University of Heidelberg</s1>
<s3>DEU</s3>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="06"><s1>Institute of Environmental Physics, University of Bremen</s1>
<s3>DEU</s3>
<sZ>9 aut.</sZ>
<sZ>10 aut.</sZ>
</fA14>
<fA20><s1>463-472</s1>
</fA20>
<fA21><s1>2000</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA25 i1="01"><s1>WIT Press</s1>
<s2>Southampton</s2>
</fA25>
<fA26 i1="01"><s0>1-85312-822-8</s0>
</fA26>
<fA30 i1="01" i2="1" l="ENG"><s1>International conference on air pollution</s1>
<s2>8</s2>
<s3>Cambridge GBR</s3>
<s4>2000</s4>
</fA30>
<fA43 i1="01"><s1>INIST</s1>
<s2>Y 33598</s2>
<s5>354000097037380470</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2002 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>11 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>02-0074706</s0>
</fA47>
<fA60><s1>C</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Tropospheric NO<sub>2</sub>
 columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO<sub>2</sub>
. The measured and modelled NO<sub>2</sub>
 columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO<sub>2</sub>
 columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO<sub>2</sub>
 columns as well as the columns measured by GOME are in good agreement with NO<sub>2</sub>
 columns derived from observed NO<sub>2</sub>
 mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO<sub>2</sub>
 columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001D16C02</s0>
</fC02>
<fC02 i1="02" i2="X"><s0>001E02D04</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>08</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Air pollution</s0>
<s5>08</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Contaminación aire</s0>
<s5>08</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Qualité air</s0>
<s5>09</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Air quality</s0>
<s5>09</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Calidad aire</s0>
<s5>09</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Azote dioxyde</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>11</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Nitrogen dioxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>11</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Nitrógeno dióxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>11</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Teneur</s0>
<s5>12</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Content</s0>
<s5>12</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Proporción</s0>
<s5>12</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Variation temporelle</s0>
<s5>13</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Time variation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Variación temporal</s0>
<s5>13</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Variation spatiale</s0>
<s5>14</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Spatial variation</s0>
<s5>14</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Variación espacial</s0>
<s5>14</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Surveillance</s0>
<s5>15</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Surveillance</s0>
<s5>15</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Vigilancia</s0>
<s5>15</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Télédétection</s0>
<s5>16</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Remote sensing</s0>
<s5>16</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Teledetección</s0>
<s5>16</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Observation par satellite</s0>
<s5>17</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Satellite observation</s0>
<s5>17</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Observación por satélite</s0>
<s5>17</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Modélisation</s0>
<s5>18</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Modeling</s0>
<s5>18</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Modelización</s0>
<s5>18</s5>
</fC03>
<fN21><s1>037</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 02-0074706 INIST</NO>
<ET>Model derived tropospheric NO<sub>2</sub>
 columns compared with GOME measurements</ET>
<AU>VELDERS (G. J. M.); GRANIER (C.); PORTMANN (R. W.); PFEILSTICKER (K.); WENIG (M.); WAGNER (T.); LEUE (C.); PLATT (U.); RICHTER (A.); BURROWS (J. P.); LONGHURST (J.W.S.); BREBBIA (C.A.); POWER (H.)</AU>
<AF>Air Research Laboratory, National Institute of Public Health and the Environment/Bilthoven/Pays-Bas (1 aut.); Aeronomy Laboratory, NOAA/Boulder/Etats-Unis (1 aut., 2 aut., 3 aut., 4 aut.); Service d'Aéronomie CNRS/Paris/France (2 aut.); CIRES, University of Colorado/Boulder/Etats-Unis (2 aut.); Institut für Umweltphysik, University of Heidelberg/Allemagne (4 aut., 5 aut., 6 aut., 7 aut., 8 aut.); Institute of Environmental Physics, University of Bremen/Allemagne (9 aut., 10 aut.)</AF>
<DT>Congrès; Niveau analytique</DT>
<SO>International conference on air pollution/8/2000/Cambridge GBR; Royaume-Uni; Southampton: WIT Press; Da. 2000; Pp. 463-472; ISBN 1-85312-822-8</SO>
<LA>Anglais</LA>
<EA>Tropospheric NO<sub>2</sub>
 columns derived from measurements by the GOME satellite instrument have been compared with calculations from the global chemistry-transport model MOZART, in order to gain insights into the distribution and fate of atmospheric NO<sub>2</sub>
. The measured and modelled NO<sub>2</sub>
 columns show similar spatial and seasonal patterns, with large tropospheric column amounts over industrialized areas and small column amounts over remote areas. The comparison of the absolute values of the measured and modelled tropospheric columns are particularly dependent upon uncertainties in the derivation of the tropospheric NO<sub>2</sub>
 columns from GOME and the difficulty of modelling the boundary layer in global models. The measured tropospheric column amounts derived from GOME data are of the same order as those calculated by MOZART over the industrialized areas of the USA and Europe, but a factor of 2-3 larger for Asia. The modelled tropospheric NO<sub>2</sub>
 columns as well as the columns measured by GOME are in good agreement with NO<sub>2</sub>
 columns derived from observed NO<sub>2</sub>
 mixing ratios in the boundary layer in eastern North America. In the near future it is expected that the GOME NO<sub>2</sub>
 columns can be used to identify "hot spots" of regional air pollution on a global map, useful for assessment studies.</EA>
<CC>001D16C02; 001E02D04</CC>
<FD>Troposphère; Pollution air; Qualité air; Azote dioxyde; Teneur; Variation temporelle; Variation spatiale; Surveillance; Télédétection; Observation par satellite; Modélisation</FD>
<ED>Troposphere; Air pollution; Air quality; Nitrogen dioxide; Content; Time variation; Spatial variation; Surveillance; Remote sensing; Satellite observation; Modeling</ED>
<SD>Troposfera; Contaminación aire; Calidad aire; Nitrógeno dióxido; Proporción; Variación temporal; Variación espacial; Vigilancia; Teledetección; Observación por satélite; Modelización</SD>
<LO>INIST-Y 33598.354000097037380470</LO>
<ID>02-0074706</ID>
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Model derived tropospheric NO2 columns compared with GOME measurements

Model derived tropospheric NO2 columns compared with GOME measurements

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