MozartV1, PascalFrancis, Corpus, bibRecord, 000255

MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description

Identifieur interne : 000255 ( PascalFrancis/Corpus ); précédent : 000254; suivant : 000256

MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description

Auteurs : G. P. Brasseur ; D. A. Hauglustaine ; S. Walters ; P. J. Rasch ; J.-F. Müller ; C. Granier ; X. X. Tie

Source :

Journal of geophysical research [ 0148-0227 ] ; 1998.

RBID : Pascal:99-0063648

Descripteurs français

Pascal (Inist)
- Troposphère, Ozone, Précurseur, Modèle chimique, Modèle 3 dimensions, Phénomène transport, Echelle planétaire, Réaction chimique, Retombée atmosphérique, Variation spatiale, Variation temporelle, Modèle climat.

English descriptors

KwdEn :
- Atmospheric fallout, Chemical model, Chemical reaction, Climate models, Ozone, Planetary scale, Precursor, Spatial variation, Three dimensional model, Time variation, Transport process, Troposphere.

Abstract

We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0148-0227`
A03		`1`		`@0 J. geophys. res.`
A05				`@2 103`
A06				`@2 D21`
A08	`01`	`1`	`ENG`	`@1 MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description`
A11	`01`	`1`		`@1 BRASSEUR (G. P.)`
A11	`02`	`1`		`@1 HAUGLUSTAINE (D. A.)`
A11	`03`	`1`		`@1 WALTERS (S.)`
A11	`04`	`1`		`@1 RASCH (P. J.)`
A11	`05`	`1`		`@1 MÜLLER (J.-F.)`
A11	`06`	`1`		`@1 GRANIER (C.)`
A11	`07`	`1`		`@1 TIE (X. X.)`
A14	`01`			`@1 National Center for Atmospheric Research @2 Boulder, Colorado @3 USA @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut. @Z 7 aut.`
A14	`02`			`@1 Service d'Aéronomie du Centre National de la Recherche Scientifique @2 Paris @3 FRA @Z 2 aut. @Z 6 aut.`
A14	`03`			`@1 Belgian Institute for Space Aeronomy @2 Brussels @3 BEL @Z 5 aut.`
A14	`04`			`@1 CIRES, University of Colorado @2 Boulder, Colorado @3 USA @Z 6 aut.`
A14	`05`			`@1 NOAA Aeronomy Laboratory @2 Boulder, Colorado @3 USA @Z 6 aut.`
A20				`@1 28265-28289`
A21				`@1 1998`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 3144 @5 354000071948230200`
A44				`@0 0000 @1 © 1999 INIST-CNRS. All rights reserved.`
A45				`@0 3 p.`
A47	`01`	`1`		`@0 99-0063648`
A60				`@1 P`
A61				`@0 A`
A64		`1`		`@0 Journal of geophysical research`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.
C02	`01`	`X`		`@0 001E02D04`
C03	`01`	`X`	`FRE`	`@0 Troposphère @5 26`
C03	`01`	`X`	`ENG`	`@0 Troposphere @5 26`
C03	`01`	`X`	`SPA`	`@0 Troposfera @5 26`
C03	`02`	`X`	`FRE`	`@0 Ozone @2 NK @2 FX @5 27`
C03	`02`	`X`	`ENG`	`@0 Ozone @2 NK @2 FX @5 27`
C03	`02`	`X`	`GER`	`@0 Ozon @2 NK @2 FX @5 27`
C03	`02`	`X`	`SPA`	`@0 Ozono @2 NK @2 FX @5 27`
C03	`03`	`X`	`FRE`	`@0 Précurseur @5 28`
C03	`03`	`X`	`ENG`	`@0 Precursor @5 28`
C03	`03`	`X`	`SPA`	`@0 Precursor @5 28`
C03	`04`	`X`	`FRE`	`@0 Modèle chimique @5 29`
C03	`04`	`X`	`ENG`	`@0 Chemical model @5 29`
C03	`04`	`X`	`SPA`	`@0 Modelo químico @5 29`
C03	`05`	`X`	`FRE`	`@0 Modèle 3 dimensions @5 30`
C03	`05`	`X`	`ENG`	`@0 Three dimensional model @5 30`
C03	`05`	`X`	`SPA`	`@0 Modelo 3 dimensiones @5 30`
C03	`06`	`X`	`FRE`	`@0 Phénomène transport @5 31`
C03	`06`	`X`	`ENG`	`@0 Transport process @5 31`
C03	`06`	`X`	`GER`	`@0 Transporterscheinung @5 31`
C03	`06`	`X`	`SPA`	`@0 Fenómeno transporte @5 31`
C03	`07`	`X`	`FRE`	`@0 Echelle planétaire @5 32`
C03	`07`	`X`	`ENG`	`@0 Planetary scale @5 32`
C03	`07`	`X`	`SPA`	`@0 Escala planetaria @5 32`
C03	`08`	`X`	`FRE`	`@0 Réaction chimique @5 33`
C03	`08`	`X`	`ENG`	`@0 Chemical reaction @5 33`
C03	`08`	`X`	`GER`	`@0 Chemische Reaktion @5 33`
C03	`08`	`X`	`SPA`	`@0 Reacción química @5 33`
C03	`09`	`X`	`FRE`	`@0 Retombée atmosphérique @5 34`
C03	`09`	`X`	`ENG`	`@0 Atmospheric fallout @5 34`
C03	`09`	`X`	`SPA`	`@0 Recaída atmosférica @5 34`
C03	`10`	`X`	`FRE`	`@0 Variation spatiale @5 35`
C03	`10`	`X`	`ENG`	`@0 Spatial variation @5 35`
C03	`10`	`X`	`SPA`	`@0 Variación espacial @5 35`
C03	`11`	`X`	`FRE`	`@0 Variation temporelle @5 36`
C03	`11`	`X`	`ENG`	`@0 Time variation @5 36`
C03	`11`	`X`	`SPA`	`@0 Variación temporal @5 36`
C03	`12`	`3`	`FRE`	`@0 Modèle climat @5 84`
C03	`12`	`3`	`ENG`	`@0 Climate models @5 84`
N21				`@1 032`

Format Inist (serveur)

NO :	PASCAL 99-0063648 INIST
ET :	MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description
AU :	BRASSEUR (G. P.); HAUGLUSTAINE (D. A.); WALTERS (S.); RASCH (P. J.); MÜLLER (J.-F.); GRANIER (C.); TIE (X. X.)
AF :	National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 2 aut., 3 aut., 4 aut., 7 aut.); Service d'Aéronomie du Centre National de la Recherche Scientifique/Paris/France (2 aut., 6 aut.); Belgian Institute for Space Aeronomy/Brussels/Belgique (5 aut.); CIRES, University of Colorado/Boulder, Colorado/Etats-Unis (6 aut.); NOAA Aeronomy Laboratory/Boulder, Colorado/Etats-Unis (6 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 1998; Vol. 103; No. D21; Pp. 28265-28289; Bibl. 3 p.
LA :	Anglais
EA :	We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.
CC :	001E02D04
FD :	Troposphère; Ozone; Précurseur; Modèle chimique; Modèle 3 dimensions; Phénomène transport; Echelle planétaire; Réaction chimique; Retombée atmosphérique; Variation spatiale; Variation temporelle; Modèle climat
ED :	Troposphere; Ozone; Precursor; Chemical model; Three dimensional model; Transport process; Planetary scale; Chemical reaction; Atmospheric fallout; Spatial variation; Time variation; Climate models
GD :	Ozon; Transporterscheinung; Chemische Reaktion
SD :	Troposfera; Ozono; Precursor; Modelo químico; Modelo 3 dimensiones; Fenómeno transporte; Escala planetaria; Reacción química; Recaída atmosférica; Variación espacial; Variación temporal
LO :	INIST-3144.354000071948230200
ID :	99-0063648

Links to Exploration step

Pascal:99-0063648

Le document en format XML

<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description</title>
<author><name sortKey="Brasseur, G P" sort="Brasseur, G P" uniqKey="Brasseur G" first="G. P." last="Brasseur">G. P. Brasseur</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Hauglustaine, D A" sort="Hauglustaine, D A" uniqKey="Hauglustaine D" first="D. A." last="Hauglustaine">D. A. Hauglustaine</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Walters, S" sort="Walters, S" uniqKey="Walters S" first="S." last="Walters">S. Walters</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Rasch, P J" sort="Rasch, P J" uniqKey="Rasch P" first="P. J." last="Rasch">P. J. Rasch</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Muller, J F" sort="Muller, J F" uniqKey="Muller J" first="J.-F." last="Müller">J.-F. Müller</name>
<affiliation><inist:fA14 i1="03"><s1>Belgian Institute for Space Aeronomy</s1>
<s2>Brussels</s2>
<s3>BEL</s3>
<sZ>5 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Granier, C" sort="Granier, C" uniqKey="Granier C" first="C." last="Granier">C. Granier</name>
<affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="04"><s1>CIRES, University of Colorado</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="05"><s1>NOAA Aeronomy Laboratory</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Tie, X X" sort="Tie, X X" uniqKey="Tie X" first="X. X." last="Tie">X. X. Tie</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">INIST</idno>
<idno type="inist">99-0063648</idno>
<date when="1998">1998</date>
<idno type="stanalyst">PASCAL 99-0063648 INIST</idno>
<idno type="RBID">Pascal:99-0063648</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000255</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description</title>
<author><name sortKey="Brasseur, G P" sort="Brasseur, G P" uniqKey="Brasseur G" first="G. P." last="Brasseur">G. P. Brasseur</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Hauglustaine, D A" sort="Hauglustaine, D A" uniqKey="Hauglustaine D" first="D. A." last="Hauglustaine">D. A. Hauglustaine</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Walters, S" sort="Walters, S" uniqKey="Walters S" first="S." last="Walters">S. Walters</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Rasch, P J" sort="Rasch, P J" uniqKey="Rasch P" first="P. J." last="Rasch">P. J. Rasch</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Muller, J F" sort="Muller, J F" uniqKey="Muller J" first="J.-F." last="Müller">J.-F. Müller</name>
<affiliation><inist:fA14 i1="03"><s1>Belgian Institute for Space Aeronomy</s1>
<s2>Brussels</s2>
<s3>BEL</s3>
<sZ>5 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Granier, C" sort="Granier, C" uniqKey="Granier C" first="C." last="Granier">C. Granier</name>
<affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="04"><s1>CIRES, University of Colorado</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="05"><s1>NOAA Aeronomy Laboratory</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Tie, X X" sort="Tie, X X" uniqKey="Tie X" first="X. X." last="Tie">X. X. Tie</name>
<affiliation><inist:fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Journal of geophysical research</title>
<title level="j" type="abbreviated">J. geophys. res.</title>
<idno type="ISSN">0148-0227</idno>
<imprint><date when="1998">1998</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Journal of geophysical research</title>
<title level="j" type="abbreviated">J. geophys. res.</title>
<idno type="ISSN">0148-0227</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Atmospheric fallout</term>
<term>Chemical model</term>
<term>Chemical reaction</term>
<term>Climate models</term>
<term>Ozone</term>
<term>Planetary scale</term>
<term>Precursor</term>
<term>Spatial variation</term>
<term>Three dimensional model</term>
<term>Time variation</term>
<term>Transport process</term>
<term>Troposphere</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Troposphère</term>
<term>Ozone</term>
<term>Précurseur</term>
<term>Modèle chimique</term>
<term>Modèle 3 dimensions</term>
<term>Phénomène transport</term>
<term>Echelle planétaire</term>
<term>Réaction chimique</term>
<term>Retombée atmosphérique</term>
<term>Variation spatiale</term>
<term>Variation temporelle</term>
<term>Modèle climat</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0148-0227</s0>
</fA01>
<fA03 i2="1"><s0>J. geophys. res.</s0>
</fA03>
<fA05><s2>103</s2>
</fA05>
<fA06><s2>D21</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>BRASSEUR (G. P.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>HAUGLUSTAINE (D. A.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>WALTERS (S.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>RASCH (P. J.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>MÜLLER (J.-F.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>GRANIER (C.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>TIE (X. X.)</s1>
</fA11>
<fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Belgian Institute for Space Aeronomy</s1>
<s2>Brussels</s2>
<s3>BEL</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>CIRES, University of Colorado</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>NOAA Aeronomy Laboratory</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA20><s1>28265-28289</s1>
</fA20>
<fA21><s1>1998</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>3144</s2>
<s5>354000071948230200</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 1999 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>99-0063648</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i2="1"><s0>Journal of geophysical research</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>001E02D04</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Troposphère</s0>
<s5>26</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Troposphere</s0>
<s5>26</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Troposfera</s0>
<s5>26</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>27</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Ozone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>27</s5>
</fC03>
<fC03 i1="02" i2="X" l="GER"><s0>Ozon</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>27</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Ozono</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>27</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Précurseur</s0>
<s5>28</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Precursor</s0>
<s5>28</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Precursor</s0>
<s5>28</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Modèle chimique</s0>
<s5>29</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Chemical model</s0>
<s5>29</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Modelo químico</s0>
<s5>29</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Modèle 3 dimensions</s0>
<s5>30</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Three dimensional model</s0>
<s5>30</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Modelo 3 dimensiones</s0>
<s5>30</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Phénomène transport</s0>
<s5>31</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Transport process</s0>
<s5>31</s5>
</fC03>
<fC03 i1="06" i2="X" l="GER"><s0>Transporterscheinung</s0>
<s5>31</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Fenómeno transporte</s0>
<s5>31</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Echelle planétaire</s0>
<s5>32</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Planetary scale</s0>
<s5>32</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Escala planetaria</s0>
<s5>32</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Réaction chimique</s0>
<s5>33</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Chemical reaction</s0>
<s5>33</s5>
</fC03>
<fC03 i1="08" i2="X" l="GER"><s0>Chemische Reaktion</s0>
<s5>33</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Reacción química</s0>
<s5>33</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Retombée atmosphérique</s0>
<s5>34</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Atmospheric fallout</s0>
<s5>34</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Recaída atmosférica</s0>
<s5>34</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Variation spatiale</s0>
<s5>35</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Spatial variation</s0>
<s5>35</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Variación espacial</s0>
<s5>35</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Variation temporelle</s0>
<s5>36</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Time variation</s0>
<s5>36</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Variación temporal</s0>
<s5>36</s5>
</fC03>
<fC03 i1="12" i2="3" l="FRE"><s0>Modèle climat</s0>
<s5>84</s5>
</fC03>
<fC03 i1="12" i2="3" l="ENG"><s0>Climate models</s0>
<s5>84</s5>
</fC03>
<fN21><s1>032</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 99-0063648 INIST</NO>
<ET>MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description</ET>
<AU>BRASSEUR (G. P.); HAUGLUSTAINE (D. A.); WALTERS (S.); RASCH (P. J.); MÜLLER (J.-F.); GRANIER (C.); TIE (X. X.)</AU>
<AF>National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 2 aut., 3 aut., 4 aut., 7 aut.); Service d'Aéronomie du Centre National de la Recherche Scientifique/Paris/France (2 aut., 6 aut.); Belgian Institute for Space Aeronomy/Brussels/Belgique (5 aut.); CIRES, University of Colorado/Boulder, Colorado/Etats-Unis (6 aut.); NOAA Aeronomy Laboratory/Boulder, Colorado/Etats-Unis (6 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 1998; Vol. 103; No. D21; Pp. 28265-28289; Bibl. 3 p.</SO>
<LA>Anglais</LA>
<EA>We present a new global three-dimensional chemical-transport model (called MOZART) developed in the framework of the NCAR Community Climate Model (CCM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors. The model, developed with a horizontal resolution of 2.8° in longitude and latitude, includes 25 levels in the vertical between the Earth's surface and an upper boundary located at approximately 35 km altitude. In its present configuration the model calculates the global distribution of 56 chemical constituents with a timestep of 20 min, and accounts for surface emission and deposition, large-scale advective transport, subscale convective and boundary layer exchanges, chemical and photochemical transformations, as well as wet scavenging. Transport is simulated "off line" from CCM with dynamical variables provided every 3 hours from preestablished history tapes. Advection is calculated using the semi-Lagrangian transport scheme [Rasch and Williamson, 1990] developed for the MATCH model of Rasch et al. [1997]. Convective and boundary layer transports are expressed according to Hack [1994] and Holtslag and Boville [1993], respectively. A detailed evaluation of the model results is provided in a companion paper [Hauglustaine et al., this issue]. An analysis of the spatial and temporal variability in the chemical fields predicted by the model suggests that regional events such as summertime ozone episodes in polluted areas can be simulated by MOZART.</EA>
<CC>001E02D04</CC>
<FD>Troposphère; Ozone; Précurseur; Modèle chimique; Modèle 3 dimensions; Phénomène transport; Echelle planétaire; Réaction chimique; Retombée atmosphérique; Variation spatiale; Variation temporelle; Modèle climat</FD>
<ED>Troposphere; Ozone; Precursor; Chemical model; Three dimensional model; Transport process; Planetary scale; Chemical reaction; Atmospheric fallout; Spatial variation; Time variation; Climate models</ED>
<GD>Ozon; Transporterscheinung; Chemische Reaktion</GD>
<SD>Troposfera; Ozono; Precursor; Modelo químico; Modelo 3 dimensiones; Fenómeno transporte; Escala planetaria; Reacción química; Recaída atmosférica; Variación espacial; Variación temporal</SD>
<LO>INIST-3144.354000071948230200</LO>
<ID>99-0063648</ID>
</server>
</inist>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Musique/explor/MozartV1/Data/PascalFrancis/Corpus

HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000255 | SxmlIndent | more

HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 000255 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Musique
   |area=    MozartV1
   |flux=    PascalFrancis
   |étape=   Corpus
   |type=    RBID
   |clé=     Pascal:99-0063648
   |texte=   MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description
}}

This area was generated with Dilib version V0.6.20.
Data generation: Sun Apr 10 15:06:14 2016. Site generation: Tue Feb 7 15:40:35 2023

	Serveur d'exploration sur Mozart
	Attention, ce site est en cours de développement ! Attention, site généré par des moyens informatiques à partir de corpus bruts. Les informations ne sont donc pas validées.

Serveur d'exploration sur Mozart

MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description

MOZART, a global chemical transport model for ozone and related chemical tracers. 1. Model description

Source :

Descripteurs français

English descriptors

Abstract

Notice en format standard (ISO 2709)

Format Inist (serveur)

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri