MozartV1, PascalFrancis, Corpus, bibRecord, 000149

Impact of climate change on the future chemical composition of the global troposphere

Identifieur interne : 000149 ( PascalFrancis/Corpus ); précédent : 000148; suivant : 000150

Impact of climate change on the future chemical composition of the global troposphere

Auteurs : Guy P. Brasseur ; Martin Schultz ; Claire Granier ; Marielle Saunois ; Thomas Diehl ; Michael Botzet ; Erich Roeckner ; Stacy Walters

Source :

Journal of climate [ 0894-8755 ] ; 2006.

RBID : Pascal:06-0480247

Descripteurs français

Pascal (Inist)
- Changement planétaire, Modification climat, Troposphère, Chimie atmosphérique, Ozone, Modèle prévision, Siècle 21eme, Simulation numérique, Modèle circulation générale, Modèle atmosphère océan, Emission polluant, Facteur anthropique, Facteur biogène, Climatologie dynamique, Modèle ECHAM5.

English descriptors

KwdEn :
- Anthropogenic factor, Atmospheric chemistry, Biogenic factor, Century 21st, Dynamical climatology, Forecast model, General circulation models, Ocean-atmosphere model, Pollutant emission, climate modification, digital simulation, global change, ozone, troposphere.

Abstract

A global chemical transport model of the atmosphere [the Model for Ozone and Related Tracers, version 2 (MOZART-2)] driven by prescribed surface emissions and by meteorological fields provided by the ECHAM5/Max Planck Institute Ocean Model (MPI-OM-1) coupled atmosphere-ocean model is used to assess how expected climate changes (2100 versus 2000 periods) should affect the chemical composition of the troposphere. Calculations suggest that ozone changes resulting from climate change only are negative in a large fraction of the troposphere because of enhanced photochemical destruction by water vapor. In the Tropics, increased lightning activity should lead to larger ozone concentrations. The magnitude of the climate-induced ozone changes in the troposphere remains smaller than the changes produced by enhanced anthropogenic emissions when the Special Report on Emission Scenarios (SRES) A2P is adopted to describe the future evolution of these emissions. Predictions depend strongly on future trends in atmospheric methane levels, which are not well established. Changes in the emissions of NOx by bacteria in soils and of nonmethane hydrocarbons by vegetation associated with climate change could have a significant impact on future ozone levels.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A11	`06`	`1`		`@1 BOTZET (Michael)`
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C01	`01`		`ENG`	@0 A global chemical transport model of the atmosphere [the Model for Ozone and Related Tracers, version 2 (MOZART-2)] driven by prescribed surface emissions and by meteorological fields provided by the ECHAM5/Max Planck Institute Ocean Model (MPI-OM-1) coupled atmosphere-ocean model is used to assess how expected climate changes (2100 versus 2000 periods) should affect the chemical composition of the troposphere. Calculations suggest that ozone changes resulting from climate change only are negative in a large fraction of the troposphere because of enhanced photochemical destruction by water vapor. In the Tropics, increased lightning activity should lead to larger ozone concentrations. The magnitude of the climate-induced ozone changes in the troposphere remains smaller than the changes produced by enhanced anthropogenic emissions when the Special Report on Emission Scenarios (SRES) A2P is adopted to describe the future evolution of these emissions. Predictions depend strongly on future trends in atmospheric methane levels, which are not well established. Changes in the emissions of NOx by bacteria in soils and of nonmethane hydrocarbons by vegetation associated with climate change could have a significant impact on future ozone levels.
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C02	`02`	`2`		`@0 001E02F`
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C03	`08`	`2`	`ENG`	`@0 digital simulation @5 08`
C03	`08`	`2`	`SPA`	`@0 Simulación numérica @5 08`
C03	`09`	`3`	`FRE`	`@0 Modèle circulation générale @5 09`
C03	`09`	`3`	`ENG`	`@0 General circulation models @5 09`
C03	`10`	`3`	`FRE`	`@0 Modèle atmosphère océan @5 10`
C03	`10`	`3`	`ENG`	`@0 Ocean-atmosphere model @5 10`
C03	`11`	`X`	`FRE`	`@0 Emission polluant @5 11`
C03	`11`	`X`	`ENG`	`@0 Pollutant emission @5 11`
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Format Inist (serveur)

NO :	PASCAL 06-0480247 INIST
ET :	Impact of climate change on the future chemical composition of the global troposphere
AU :	BRASSEUR (Guy P.); SCHULTZ (Martin); GRANIER (Claire); SAUNOIS (Marielle); DIEHL (Thomas); BOTZET (Michael); ROECKNER (Erich); WALTERS (Stacy)
AF :	Max Planck Institute for Meteorology/Hamburg/Allemagne (1 aut., 2 aut., 3 aut., 4 aut., 5 aut., 6 aut., 7 aut.); National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (8 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of climate; ISSN 0894-8755; Etats-Unis; Da. 2006; Vol. 19; No. 16; Pp. 3932-3951; Bibl. 1 p.3/4
LA :	Anglais
EA :	A global chemical transport model of the atmosphere [the Model for Ozone and Related Tracers, version 2 (MOZART-2)] driven by prescribed surface emissions and by meteorological fields provided by the ECHAM5/Max Planck Institute Ocean Model (MPI-OM-1) coupled atmosphere-ocean model is used to assess how expected climate changes (2100 versus 2000 periods) should affect the chemical composition of the troposphere. Calculations suggest that ozone changes resulting from climate change only are negative in a large fraction of the troposphere because of enhanced photochemical destruction by water vapor. In the Tropics, increased lightning activity should lead to larger ozone concentrations. The magnitude of the climate-induced ozone changes in the troposphere remains smaller than the changes produced by enhanced anthropogenic emissions when the Special Report on Emission Scenarios (SRES) A2P is adopted to describe the future evolution of these emissions. Predictions depend strongly on future trends in atmospheric methane levels, which are not well established. Changes in the emissions of NOx by bacteria in soils and of nonmethane hydrocarbons by vegetation associated with climate change could have a significant impact on future ozone levels.
CC :	001E02D10; 001E02F
FD :	Changement planétaire; Modification climat; Troposphère; Chimie atmosphérique; Ozone; Modèle prévision; Siècle 21eme; Simulation numérique; Modèle circulation générale; Modèle atmosphère océan; Emission polluant; Facteur anthropique; Facteur biogène; Climatologie dynamique; Modèle ECHAM5
ED :	global change; climate modification; troposphere; Atmospheric chemistry; ozone; Forecast model; Century 21st; digital simulation; General circulation models; Ocean-atmosphere model; Pollutant emission; Anthropogenic factor; Biogenic factor; Dynamical climatology
SD :	Cambio planetario; Ozono; Modelo previsión; Siglo 21; Simulación numérica; Emisión contaminante; Factor antrópico; Factor biógeno; Climatología dinámica
LO :	INIST-9644B.354000133590630090
ID :	06-0480247

Links to Exploration step

Pascal:06-0480247

Le document en format XML

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<term>Dynamical climatology</term>
<term>Forecast model</term>
<term>General circulation models</term>
<term>Ocean-atmosphere model</term>
<term>Pollutant emission</term>
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<term>Modèle prévision</term>
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<term>Modèle atmosphère océan</term>
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<front><div type="abstract" xml:lang="en">A global chemical transport model of the atmosphere [the Model for Ozone and Related Tracers, version 2 (MOZART-2)] driven by prescribed surface emissions and by meteorological fields provided by the ECHAM5/Max Planck Institute Ocean Model (MPI-OM-1) coupled atmosphere-ocean model is used to assess how expected climate changes (2100 versus 2000 periods) should affect the chemical composition of the troposphere. Calculations suggest that ozone changes resulting from climate change only are negative in a large fraction of the troposphere because of enhanced photochemical destruction by water vapor. In the Tropics, increased lightning activity should lead to larger ozone concentrations. The magnitude of the climate-induced ozone changes in the troposphere remains smaller than the changes produced by enhanced anthropogenic emissions when the Special Report on Emission Scenarios (SRES) A2P is adopted to describe the future evolution of these emissions. Predictions depend strongly on future trends in atmospheric methane levels, which are not well established. Changes in the emissions of NOx by bacteria in soils and of nonmethane hydrocarbons by vegetation associated with climate change could have a significant impact on future ozone levels.</div>
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<fA11 i1="08" i2="1"><s1>WALTERS (Stacy)</s1>
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<fA14 i1="01"><s1>Max Planck Institute for Meteorology</s1>
<s2>Hamburg</s2>
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<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>8 aut.</sZ>
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<fA20><s1>3932-3951</s1>
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<fC03 i1="06" i2="X" l="FRE"><s0>Modèle prévision</s0>
<s5>06</s5>
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<s5>09</s5>
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<s5>09</s5>
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<fC03 i1="10" i2="3" l="FRE"><s0>Modèle atmosphère océan</s0>
<s5>10</s5>
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<s5>10</s5>
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<s5>11</s5>
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<s5>12</s5>
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<s5>12</s5>
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<s5>13</s5>
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<s5>13</s5>
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<s5>31</s5>
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<fC03 i1="14" i2="X" l="ENG"><s0>Dynamical climatology</s0>
<s5>31</s5>
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<fC03 i1="14" i2="X" l="SPA"><s0>Climatología dinámica</s0>
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<fC03 i1="15" i2="2" l="FRE"><s0>Modèle ECHAM5</s0>
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<server><NO>PASCAL 06-0480247 INIST</NO>
<ET>Impact of climate change on the future chemical composition of the global troposphere</ET>
<AU>BRASSEUR (Guy P.); SCHULTZ (Martin); GRANIER (Claire); SAUNOIS (Marielle); DIEHL (Thomas); BOTZET (Michael); ROECKNER (Erich); WALTERS (Stacy)</AU>
<AF>Max Planck Institute for Meteorology/Hamburg/Allemagne (1 aut., 2 aut., 3 aut., 4 aut., 5 aut., 6 aut., 7 aut.); National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (8 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of climate; ISSN 0894-8755; Etats-Unis; Da. 2006; Vol. 19; No. 16; Pp. 3932-3951; Bibl. 1 p.3/4</SO>
<LA>Anglais</LA>
<EA>A global chemical transport model of the atmosphere [the Model for Ozone and Related Tracers, version 2 (MOZART-2)] driven by prescribed surface emissions and by meteorological fields provided by the ECHAM5/Max Planck Institute Ocean Model (MPI-OM-1) coupled atmosphere-ocean model is used to assess how expected climate changes (2100 versus 2000 periods) should affect the chemical composition of the troposphere. Calculations suggest that ozone changes resulting from climate change only are negative in a large fraction of the troposphere because of enhanced photochemical destruction by water vapor. In the Tropics, increased lightning activity should lead to larger ozone concentrations. The magnitude of the climate-induced ozone changes in the troposphere remains smaller than the changes produced by enhanced anthropogenic emissions when the Special Report on Emission Scenarios (SRES) A2P is adopted to describe the future evolution of these emissions. Predictions depend strongly on future trends in atmospheric methane levels, which are not well established. Changes in the emissions of NOx by bacteria in soils and of nonmethane hydrocarbons by vegetation associated with climate change could have a significant impact on future ozone levels.</EA>
<CC>001E02D10; 001E02F</CC>
<FD>Changement planétaire; Modification climat; Troposphère; Chimie atmosphérique; Ozone; Modèle prévision; Siècle 21eme; Simulation numérique; Modèle circulation générale; Modèle atmosphère océan; Emission polluant; Facteur anthropique; Facteur biogène; Climatologie dynamique; Modèle ECHAM5</FD>
<ED>global change; climate modification; troposphere; Atmospheric chemistry; ozone; Forecast model; Century 21st; digital simulation; General circulation models; Ocean-atmosphere model; Pollutant emission; Anthropogenic factor; Biogenic factor; Dynamical climatology</ED>
<SD>Cambio planetario; Ozono; Modelo previsión; Siglo 21; Simulación numérica; Emisión contaminante; Factor antrópico; Factor biógeno; Climatología dinámica</SD>
<LO>INIST-9644B.354000133590630090</LO>
<ID>06-0480247</ID>
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Impact of climate change on the future chemical composition of the global troposphere

Impact of climate change on the future chemical composition of the global troposphere

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