MozartV1, PascalFrancis, Corpus, bibRecord, 000244

A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions

Identifieur interne : 000244 ( PascalFrancis/Corpus ); précédent : 000243; suivant : 000245

A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions

Auteurs : D. A. Hauglustaine ; G. P. Brasseur ; J. S. Levine

Source :

Geophysical research letters [ 0094-8276 ] ; 1999.

RBID : Pascal:00-0003289

Descripteurs français

Pascal (Inist)
- Troposphère, Ozone, Feu végétation, Simulation numérique, Analyse sensibilité, Photochimie, Précurseur, Carbone monoxyde, Rapport mélange, Densité colonne, Phénomène transport, Indonésie.

English descriptors

KwdEn :
- Canopy fire, Carbon monoxide, Column density, Indonesia, Mixing ratio, Numerical simulation, Ozone, Photochemistry, Precursor, Sensitivity analysis, Transport process, Troposphere.

Abstract

A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O₃ column increases by 20-25 DU and the ozone mixing ratio reaches 50 ppbv in the mid-troposphere in November. South of the source region, low ozone mixing ratios of 20-25 ppbv are calculated in the boundary layer due to marine air influence and reduced photochemical activity in presence of biomass burning aerosols. The particular transport regime prevailing during the 1997 El Niño event is not considered in our calculations. This limitation precludes any definitive conclusion regarding the relative role played by photochemistry and transport processes on the distribution of species during the 1997 fires.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0094-8276`
A02	`01`			`@0 GPRLAJ`
A03		`1`		`@0 Geophys. res. lett.`
A05				`@2 26`
A06				`@2 21`
A08	`01`	`1`	`ENG`	`@1 A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions`
A11	`01`	`1`		`@1 HAUGLUSTAINE (D. A.)`
A11	`02`	`1`		`@1 BRASSEUR (G. P.)`
A11	`03`	`1`		`@1 LEVINE (J. S.)`
A14	`01`			`@1 Service d'Aéronomie du CNRS, Université de Paris 6 @2 Paris @3 FRA @Z 1 aut.`
A14	`02`			`@1 National Center for Atmospheric Research @2 Boulder, CO @3 USA @Z 2 aut.`
A14	`03`			`@1 Atmospheric Sciences Division, NASA Langley Research Center @2 Hampton, VA @3 USA @Z 3 aut.`
A20				`@1 3305-3308`
A21				`@1 1999`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 16687 @5 354000080439380250`
A44				`@0 0000 @1 © 2000 INIST-CNRS. All rights reserved.`
A45				`@0 13 ref.`
A47	`01`	`1`		`@0 00-0003289`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Geophysical research letters`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O₃ column increases by 20-25 DU and the ozone mixing ratio reaches 50 ppbv in the mid-troposphere in November. South of the source region, low ozone mixing ratios of 20-25 ppbv are calculated in the boundary layer due to marine air influence and reduced photochemical activity in presence of biomass burning aerosols. The particular transport regime prevailing during the 1997 El Niño event is not considered in our calculations. This limitation precludes any definitive conclusion regarding the relative role played by photochemistry and transport processes on the distribution of species during the 1997 fires.
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`	`SPA`	`@0 Ozono @2 NK @2 FX @5 27`
C03	`03`	`X`	`FRE`	`@0 Feu végétation @5 28`
C03	`03`	`X`	`ENG`	`@0 Canopy fire @5 28`
C03	`03`	`X`	`SPA`	`@0 Fuego vegetación @5 28`
C03	`04`	`X`	`FRE`	`@0 Simulation numérique @5 29`
C03	`04`	`X`	`ENG`	`@0 Numerical simulation @5 29`
C03	`04`	`X`	`SPA`	`@0 Simulación numérica @5 29`
C03	`05`	`X`	`FRE`	`@0 Analyse sensibilité @5 30`
C03	`05`	`X`	`ENG`	`@0 Sensitivity analysis @5 30`
C03	`05`	`X`	`SPA`	`@0 Análisis sensibilidad @5 30`
C03	`06`	`X`	`FRE`	`@0 Photochimie @5 31`
C03	`06`	`X`	`ENG`	`@0 Photochemistry @5 31`
C03	`06`	`X`	`SPA`	`@0 Fotoquímica @5 31`
C03	`07`	`X`	`FRE`	`@0 Précurseur @5 32`
C03	`07`	`X`	`ENG`	`@0 Precursor @5 32`
C03	`07`	`X`	`SPA`	`@0 Precursor @5 32`
C03	`08`	`X`	`FRE`	`@0 Carbone monoxyde @2 NK @2 FX @5 33`
C03	`08`	`X`	`ENG`	`@0 Carbon monoxide @2 NK @2 FX @5 33`
C03	`08`	`X`	`SPA`	`@0 Carbono monóxido @2 NK @2 FX @5 33`
C03	`09`	`X`	`FRE`	`@0 Rapport mélange @5 34`
C03	`09`	`X`	`ENG`	`@0 Mixing ratio @5 34`
C03	`09`	`X`	`SPA`	`@0 Relación mezcla @5 34`
C03	`10`	`X`	`FRE`	`@0 Densité colonne @5 35`
C03	`10`	`X`	`ENG`	`@0 Column density @5 35`
C03	`10`	`X`	`SPA`	`@0 Densidad columna @5 35`
C03	`11`	`X`	`FRE`	`@0 Phénomène transport @5 36`
C03	`11`	`X`	`ENG`	`@0 Transport process @5 36`
C03	`11`	`X`	`SPA`	`@0 Fenómeno transporte @5 36`
C03	`12`	`X`	`FRE`	`@0 Indonésie @2 NG @5 46`
C03	`12`	`X`	`ENG`	`@0 Indonesia @2 NG @5 46`
C03	`12`	`X`	`SPA`	`@0 Indonesia @2 NG @5 46`
C07	`01`	`X`	`FRE`	`@0 Asie @2 NG`
C07	`01`	`X`	`ENG`	`@0 Asia @2 NG`
C07	`01`	`X`	`SPA`	`@0 Asia @2 NG`
N21				`@1 003`

Format Inist (serveur)

NO :	PASCAL 00-0003289 INIST
ET :	A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions
AU :	HAUGLUSTAINE (D. A.); BRASSEUR (G. P.); LEVINE (J. S.)
AF :	Service d'Aéronomie du CNRS, Université de Paris 6/Paris/France (1 aut.); National Center for Atmospheric Research/Boulder, CO/Etats-Unis (2 aut.); Atmospheric Sciences Division, NASA Langley Research Center/Hampton, VA/Etats-Unis (3 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 1999; Vol. 26; No. 21; Pp. 3305-3308; Bibl. 13 ref.
LA :	Anglais
EA :	A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O₃ column increases by 20-25 DU and the ozone mixing ratio reaches 50 ppbv in the mid-troposphere in November. South of the source region, low ozone mixing ratios of 20-25 ppbv are calculated in the boundary layer due to marine air influence and reduced photochemical activity in presence of biomass burning aerosols. The particular transport regime prevailing during the 1997 El Niño event is not considered in our calculations. This limitation precludes any definitive conclusion regarding the relative role played by photochemistry and transport processes on the distribution of species during the 1997 fires.
CC :	001E02D04
FD :	Troposphère; Ozone; Feu végétation; Simulation numérique; Analyse sensibilité; Photochimie; Précurseur; Carbone monoxyde; Rapport mélange; Densité colonne; Phénomène transport; Indonésie
FG :	Asie
ED :	Troposphere; Ozone; Canopy fire; Numerical simulation; Sensitivity analysis; Photochemistry; Precursor; Carbon monoxide; Mixing ratio; Column density; Transport process; Indonesia
EG :	Asia
SD :	Troposfera; Ozono; Fuego vegetación; Simulación numérica; Análisis sensibilidad; Fotoquímica; Precursor; Carbono monóxido; Relación mezcla; Densidad columna; Fenómeno transporte; Indonesia
LO :	INIST-16687.354000080439380250
ID :	00-0003289

Links to Exploration step

Pascal:00-0003289

Le document en format XML

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<front><div type="abstract" xml:lang="en">A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O<sub>3</sub>
 column increases by 20-25 DU and the ozone mixing ratio reaches 50 ppbv in the mid-troposphere in November. South of the source region, low ozone mixing ratios of 20-25 ppbv are calculated in the boundary layer due to marine air influence and reduced photochemical activity in presence of biomass burning aerosols. The particular transport regime prevailing during the 1997 El Niño event is not considered in our calculations. This limitation precludes any definitive conclusion regarding the relative role played by photochemistry and transport processes on the distribution of species during the 1997 fires.</div>
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<fC01 i1="01" l="ENG"><s0>A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O<sub>3</sub>
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<s5>34</s5>
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<s5>34</s5>
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<s5>35</s5>
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<s5>35</s5>
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<s5>35</s5>
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<fC03 i1="11" i2="X" l="FRE"><s0>Phénomène transport</s0>
<s5>36</s5>
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<s5>36</s5>
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<s5>36</s5>
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<s5>46</s5>
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<fC03 i1="12" i2="X" l="SPA"><s0>Indonesia</s0>
<s2>NG</s2>
<s5>46</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Asie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Asia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Asia</s0>
<s2>NG</s2>
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<fN21><s1>003</s1>
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<server><NO>PASCAL 00-0003289 INIST</NO>
<ET>A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions</ET>
<AU>HAUGLUSTAINE (D. A.); BRASSEUR (G. P.); LEVINE (J. S.)</AU>
<AF>Service d'Aéronomie du CNRS, Université de Paris 6/Paris/France (1 aut.); National Center for Atmospheric Research/Boulder, CO/Etats-Unis (2 aut.); Atmospheric Sciences Division, NASA Langley Research Center/Hampton, VA/Etats-Unis (3 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 1999; Vol. 26; No. 21; Pp. 3305-3308; Bibl. 13 ref.</SO>
<LA>Anglais</LA>
<EA>A global chemical transport model, called MOZART, is used to investigate the photochemical impact of the 1997 Indonesian fires on tropospheric ozone and its precursors in the tropics. Due to the high release of carbon monoxide by peat fires, CO increases by up to 1000 ppbv in the free troposphere over Indonesia. As a consequence of increased photochemical production, ozone is significantly perturbed over source regions (Sumatra and Kalimantan). The tropospheric O<sub>3</sub>
 column increases by 20-25 DU and the ozone mixing ratio reaches 50 ppbv in the mid-troposphere in November. South of the source region, low ozone mixing ratios of 20-25 ppbv are calculated in the boundary layer due to marine air influence and reduced photochemical activity in presence of biomass burning aerosols. The particular transport regime prevailing during the 1997 El Niño event is not considered in our calculations. This limitation precludes any definitive conclusion regarding the relative role played by photochemistry and transport processes on the distribution of species during the 1997 fires.</EA>
<CC>001E02D04</CC>
<FD>Troposphère; Ozone; Feu végétation; Simulation numérique; Analyse sensibilité; Photochimie; Précurseur; Carbone monoxyde; Rapport mélange; Densité colonne; Phénomène transport; Indonésie</FD>
<FG>Asie</FG>
<ED>Troposphere; Ozone; Canopy fire; Numerical simulation; Sensitivity analysis; Photochemistry; Precursor; Carbon monoxide; Mixing ratio; Column density; Transport process; Indonesia</ED>
<EG>Asia</EG>
<SD>Troposfera; Ozono; Fuego vegetación; Simulación numérica; Análisis sensibilidad; Fotoquímica; Precursor; Carbono monóxido; Relación mezcla; Densidad columna; Fenómeno transporte; Indonesia</SD>
<LO>INIST-16687.354000080439380250</LO>
<ID>00-0003289</ID>
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A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions

A sensitivity simulation of tropospheric ozone changes due to the 1997 Indonesian fire emissions

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