Study of tropospheric CO and O3 enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)
Identifieur interne : 000025 ( PascalFrancis/Corpus ); précédent : 000024; suivant : 000026Study of tropospheric CO and O3 enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)
Auteurs : Shuchita Srivastava ; Varun SheelSource :
- Atmospheric environment : (1994) [ 1352-2310 ] ; 2013.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
An intense biomass burning event occurred over Indonesia in Autumn of 2006. We study the impact of this event on the free tropospheric abundances of carbon monoxide (CO) and ozone (O3) using MOPITT (Measurements of Pollution In The Troposphere) observations, ozonesonde measurements and 3D chemistry transport model MOZART (Model for Ozone and Related chemical Tracers). MOPITT observations showed an episode of enhanced CO in the free troposphere over the Indonesian region during October-November 2006. This feature is reproduced well by MOZART. The model mass diagnostics identifies the source of enhanced CO mixing ratio in the free troposphere (100-250 ppbv) as due to convective processes. The implication of the fire plume on the vertical distribution of 03 over Kuala Lumpur has been studied. The tropospheric O3 increased over this location by 10-25 ppbv during Autumn 2006 as compared to Autumn 2005 and 2007. The MOZART model simulation significantly underestimated this tropospheric O3 enhancement. The model is run both with and without Indonesian biomass burning emissions to estimate the contribution of fire emission in CO and O3 enhancement. Biomass burning emission is found to be responsible for an average increase in CO by 104 ± 56 ppbv and O3 by 5 ± 1 ppbv from surface to 100 hPa range. The model results also showed that biomass burning and El Niño related dynamical changes both contributed (∼4 ppbv-12 ppbv) to the observed increase in tropospheric O3 over the Indonesian region during Autumn 2006.
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
| pA |
|
|---|
Format Inist (serveur)
| NO : | PASCAL 13-0194370 INIST |
|---|---|
| ET : | Study of tropospheric CO and O3 enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4) |
| AU : | SRIVASTAVA (Shuchita); SHEEL (Varun) |
| AF : | Physical Research Laboratory/Ahmedabad, Gujarat/Inde (1 aut., 2 aut.) |
| DT : | Publication en série; Niveau analytique |
| SO : | Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2013; Vol. 67; Pp. 53-62; Bibl. 3/4 p. |
| LA : | Anglais |
| EA : | An intense biomass burning event occurred over Indonesia in Autumn of 2006. We study the impact of this event on the free tropospheric abundances of carbon monoxide (CO) and ozone (O3) using MOPITT (Measurements of Pollution In The Troposphere) observations, ozonesonde measurements and 3D chemistry transport model MOZART (Model for Ozone and Related chemical Tracers). MOPITT observations showed an episode of enhanced CO in the free troposphere over the Indonesian region during October-November 2006. This feature is reproduced well by MOZART. The model mass diagnostics identifies the source of enhanced CO mixing ratio in the free troposphere (100-250 ppbv) as due to convective processes. The implication of the fire plume on the vertical distribution of 03 over Kuala Lumpur has been studied. The tropospheric O3 increased over this location by 10-25 ppbv during Autumn 2006 as compared to Autumn 2005 and 2007. The MOZART model simulation significantly underestimated this tropospheric O3 enhancement. The model is run both with and without Indonesian biomass burning emissions to estimate the contribution of fire emission in CO and O3 enhancement. Biomass burning emission is found to be responsible for an average increase in CO by 104 ± 56 ppbv and O3 by 5 ± 1 ppbv from surface to 100 hPa range. The model results also showed that biomass burning and El Niño related dynamical changes both contributed (∼4 ppbv-12 ppbv) to the observed increase in tropospheric O3 over the Indonesian region during Autumn 2006. |
| CC : | 001D16C02 |
| FD : | Troposphère; Ozone; Monoxyde de carbone; Traceur; Feu végétation; Biomasse; Combustion; Transport chimique; Modèle 3 dimensions; Panache; Pollution air; Distribution concentration; Indonésie; Oxydant photochimique |
| FG : | Asie |
| ED : | Troposphere; Ozone; Carbon monoxide; Tracers; Vegetation fire; Biomass; Combustion; Chemical transport; Three dimensional model; Plume; Air pollution; Concentration distribution; Indonesia; Photochemical oxidants |
| EG : | Asia |
| SD : | Troposfera; Ozono; Carbono monóxido; Trazador; Fuego vegetación; Biomasa; Combustión; Transporte químico; Modelo 3 dimensiones; Penacho; Contaminación aire; Distribución concentración; Indonesia |
| LO : | INIST-8940B.354000506371730070 |
| ID : | 13-0194370 |
Links to Exploration step
Pascal:13-0194370Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Study of tropospheric CO and O<sub>3</sub> enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)</title><author><name sortKey="Srivastava, Shuchita" sort="Srivastava, Shuchita" uniqKey="Srivastava S" first="Shuchita" last="Srivastava">Shuchita Srivastava</name><affiliation><inist:fA14 i1="01"><s1>Physical Research Laboratory</s1><s2>Ahmedabad, Gujarat</s2><s3>IND</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Sheel, Varun" sort="Sheel, Varun" uniqKey="Sheel V" first="Varun" last="Sheel">Varun Sheel</name><affiliation><inist:fA14 i1="01"><s1>Physical Research Laboratory</s1><s2>Ahmedabad, Gujarat</s2><s3>IND</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">13-0194370</idno><date when="2013">2013</date><idno type="stanalyst">PASCAL 13-0194370 INIST</idno><idno type="RBID">Pascal:13-0194370</idno><idno type="wicri:Area/PascalFrancis/Corpus">000025</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Study of tropospheric CO and O<sub>3</sub> enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)</title><author><name sortKey="Srivastava, Shuchita" sort="Srivastava, Shuchita" uniqKey="Srivastava S" first="Shuchita" last="Srivastava">Shuchita Srivastava</name><affiliation><inist:fA14 i1="01"><s1>Physical Research Laboratory</s1><s2>Ahmedabad, Gujarat</s2><s3>IND</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Sheel, Varun" sort="Sheel, Varun" uniqKey="Sheel V" first="Varun" last="Sheel">Varun Sheel</name><affiliation><inist:fA14 i1="01"><s1>Physical Research Laboratory</s1><s2>Ahmedabad, Gujarat</s2><s3>IND</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author></analytic><series><title level="j" type="main">Atmospheric environment : (1994)</title><title level="j" type="abbreviated">Atmos. environ. : (1994)</title><idno type="ISSN">1352-2310</idno><imprint><date when="2013">2013</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Atmospheric environment : (1994)</title><title level="j" type="abbreviated">Atmos. environ. : (1994)</title><idno type="ISSN">1352-2310</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Air pollution</term><term>Biomass</term><term>Carbon monoxide</term><term>Chemical transport</term><term>Combustion</term><term>Concentration distribution</term><term>Indonesia</term><term>Ozone</term><term>Photochemical oxidants</term><term>Plume</term><term>Three dimensional model</term><term>Tracers</term><term>Troposphere</term><term>Vegetation fire</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Troposphère</term><term>Ozone</term><term>Monoxyde de carbone</term><term>Traceur</term><term>Feu végétation</term><term>Biomasse</term><term>Combustion</term><term>Transport chimique</term><term>Modèle 3 dimensions</term><term>Panache</term><term>Pollution air</term><term>Distribution concentration</term><term>Indonésie</term><term>Oxydant photochimique</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">An intense biomass burning event occurred over Indonesia in Autumn of 2006. We study the impact of this event on the free tropospheric abundances of carbon monoxide (CO) and ozone (O<sub>3</sub>) using MOPITT (Measurements of Pollution In The Troposphere) observations, ozonesonde measurements and 3D chemistry transport model MOZART (Model for Ozone and Related chemical Tracers). MOPITT observations showed an episode of enhanced CO in the free troposphere over the Indonesian region during October-November 2006. This feature is reproduced well by MOZART. The model mass diagnostics identifies the source of enhanced CO mixing ratio in the free troposphere (100-250 ppbv) as due to convective processes. The implication of the fire plume on the vertical distribution of 0<sub>3</sub> over Kuala Lumpur has been studied. The tropospheric O<sub>3</sub> increased over this location by 10-25 ppbv during Autumn 2006 as compared to Autumn 2005 and 2007. The MOZART model simulation significantly underestimated this tropospheric O<sub>3</sub> enhancement. The model is run both with and without Indonesian biomass burning emissions to estimate the contribution of fire emission in CO and O<sub>3</sub> enhancement. Biomass burning emission is found to be responsible for an average increase in CO by 104 ± 56 ppbv and O<sub>3</sub> by 5 ± 1 ppbv from surface to 100 hPa range. The model results also showed that biomass burning and El Niño related dynamical changes both contributed (∼4 ppbv-12 ppbv) to the observed increase in tropospheric O<sub>3</sub> over the Indonesian region during Autumn 2006.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1352-2310</s0></fA01><fA03 i2="1"><s0>Atmos. environ. : (1994)</s0></fA03><fA05><s2>67</s2></fA05><fA08 i1="01" i2="1" l="ENG"><s1>Study of tropospheric CO and O<sub>3</sub> enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)</s1></fA08><fA11 i1="01" i2="1"><s1>SRIVASTAVA (Shuchita)</s1></fA11><fA11 i1="02" i2="1"><s1>SHEEL (Varun)</s1></fA11><fA14 i1="01"><s1>Physical Research Laboratory</s1><s2>Ahmedabad, Gujarat</s2><s3>IND</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></fA14><fA20><s1>53-62</s1></fA20><fA21><s1>2013</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>8940B</s2><s5>354000506371730070</s5></fA43><fA44><s0>0000</s0><s1>© 2013 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>3/4 p.</s0></fA45><fA47 i1="01" i2="1"><s0>13-0194370</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Atmospheric environment : (1994)</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fC01 i1="01" l="ENG"><s0>An intense biomass burning event occurred over Indonesia in Autumn of 2006. We study the impact of this event on the free tropospheric abundances of carbon monoxide (CO) and ozone (O<sub>3</sub>) using MOPITT (Measurements of Pollution In The Troposphere) observations, ozonesonde measurements and 3D chemistry transport model MOZART (Model for Ozone and Related chemical Tracers). MOPITT observations showed an episode of enhanced CO in the free troposphere over the Indonesian region during October-November 2006. This feature is reproduced well by MOZART. The model mass diagnostics identifies the source of enhanced CO mixing ratio in the free troposphere (100-250 ppbv) as due to convective processes. The implication of the fire plume on the vertical distribution of 0<sub>3</sub> over Kuala Lumpur has been studied. The tropospheric O<sub>3</sub> increased over this location by 10-25 ppbv during Autumn 2006 as compared to Autumn 2005 and 2007. The MOZART model simulation significantly underestimated this tropospheric O<sub>3</sub> enhancement. The model is run both with and without Indonesian biomass burning emissions to estimate the contribution of fire emission in CO and O<sub>3</sub> enhancement. Biomass burning emission is found to be responsible for an average increase in CO by 104 ± 56 ppbv and O<sub>3</sub> by 5 ± 1 ppbv from surface to 100 hPa range. The model results also showed that biomass burning and El Niño related dynamical changes both contributed (∼4 ppbv-12 ppbv) to the observed increase in tropospheric O<sub>3</sub> over the Indonesian region during Autumn 2006.</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>Ozone</s0><s2>NK</s2><s2>FX</s2><s5>02</s5></fC03><fC03 i1="02" i2="X" l="ENG"><s0>Ozone</s0><s2>NK</s2><s2>FX</s2><s5>02</s5></fC03><fC03 i1="02" i2="X" l="SPA"><s0>Ozono</s0><s2>NK</s2><s2>FX</s2><s5>02</s5></fC03><fC03 i1="03" i2="X" l="FRE"><s0>Monoxyde de carbone</s0><s2>NK</s2><s2>FX</s2><s5>03</s5></fC03><fC03 i1="03" i2="X" l="ENG"><s0>Carbon monoxide</s0><s2>NK</s2><s2>FX</s2><s5>03</s5></fC03><fC03 i1="03" i2="X" l="SPA"><s0>Carbono monóxido</s0><s2>NK</s2><s2>FX</s2><s5>03</s5></fC03><fC03 i1="04" i2="X" l="FRE"><s0>Traceur</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="ENG"><s0>Tracers</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="SPA"><s0>Trazador</s0><s5>04</s5></fC03><fC03 i1="05" i2="X" l="FRE"><s0>Feu végétation</s0><s5>05</s5></fC03><fC03 i1="05" i2="X" l="ENG"><s0>Vegetation fire</s0><s5>05</s5></fC03><fC03 i1="05" i2="X" l="SPA"><s0>Fuego vegetación</s0><s5>05</s5></fC03><fC03 i1="06" i2="X" l="FRE"><s0>Biomasse</s0><s5>06</s5></fC03><fC03 i1="06" i2="X" l="ENG"><s0>Biomass</s0><s5>06</s5></fC03><fC03 i1="06" i2="X" l="SPA"><s0>Biomasa</s0><s5>06</s5></fC03><fC03 i1="07" i2="X" l="FRE"><s0>Combustion</s0><s5>07</s5></fC03><fC03 i1="07" i2="X" l="ENG"><s0>Combustion</s0><s5>07</s5></fC03><fC03 i1="07" i2="X" l="SPA"><s0>Combustión</s0><s5>07</s5></fC03><fC03 i1="08" i2="X" l="FRE"><s0>Transport chimique</s0><s5>08</s5></fC03><fC03 i1="08" i2="X" l="ENG"><s0>Chemical transport</s0><s5>08</s5></fC03><fC03 i1="08" i2="X" l="SPA"><s0>Transporte químico</s0><s5>08</s5></fC03><fC03 i1="09" i2="X" l="FRE"><s0>Modèle 3 dimensions</s0><s5>09</s5></fC03><fC03 i1="09" i2="X" l="ENG"><s0>Three dimensional model</s0><s5>09</s5></fC03><fC03 i1="09" i2="X" l="SPA"><s0>Modelo 3 dimensiones</s0><s5>09</s5></fC03><fC03 i1="10" i2="X" l="FRE"><s0>Panache</s0><s5>10</s5></fC03><fC03 i1="10" i2="X" l="ENG"><s0>Plume</s0><s5>10</s5></fC03><fC03 i1="10" i2="X" l="SPA"><s0>Penacho</s0><s5>10</s5></fC03><fC03 i1="11" i2="X" l="FRE"><s0>Pollution air</s0><s5>11</s5></fC03><fC03 i1="11" i2="X" l="ENG"><s0>Air pollution</s0><s5>11</s5></fC03><fC03 i1="11" i2="X" l="SPA"><s0>Contaminación aire</s0><s5>11</s5></fC03><fC03 i1="12" i2="X" l="FRE"><s0>Distribution concentration</s0><s5>12</s5></fC03><fC03 i1="12" i2="X" l="ENG"><s0>Concentration distribution</s0><s5>12</s5></fC03><fC03 i1="12" i2="X" l="SPA"><s0>Distribución concentración</s0><s5>12</s5></fC03><fC03 i1="13" i2="X" l="FRE"><s0>Indonésie</s0><s2>NG</s2><s5>31</s5></fC03><fC03 i1="13" i2="X" l="ENG"><s0>Indonesia</s0><s2>NG</s2><s5>31</s5></fC03><fC03 i1="13" i2="X" l="SPA"><s0>Indonesia</s0><s2>NG</s2><s5>31</s5></fC03><fC03 i1="14" i2="3" l="FRE"><s0>Oxydant photochimique</s0><s5>35</s5></fC03><fC03 i1="14" i2="3" l="ENG"><s0>Photochemical oxidants</s0><s5>35</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></fC07><fN21><s1>175</s1></fN21></pA></standard><server><NO>PASCAL 13-0194370 INIST</NO><ET>Study of tropospheric CO and O<sub>3</sub> enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)</ET><AU>SRIVASTAVA (Shuchita); SHEEL (Varun)</AU><AF>Physical Research Laboratory/Ahmedabad, Gujarat/Inde (1 aut., 2 aut.)</AF><DT>Publication en série; Niveau analytique</DT><SO>Atmospheric environment : (1994); ISSN 1352-2310; Royaume-Uni; Da. 2013; Vol. 67; Pp. 53-62; Bibl. 3/4 p.</SO><LA>Anglais</LA><EA>An intense biomass burning event occurred over Indonesia in Autumn of 2006. We study the impact of this event on the free tropospheric abundances of carbon monoxide (CO) and ozone (O<sub>3</sub>) using MOPITT (Measurements of Pollution In The Troposphere) observations, ozonesonde measurements and 3D chemistry transport model MOZART (Model for Ozone and Related chemical Tracers). MOPITT observations showed an episode of enhanced CO in the free troposphere over the Indonesian region during October-November 2006. This feature is reproduced well by MOZART. The model mass diagnostics identifies the source of enhanced CO mixing ratio in the free troposphere (100-250 ppbv) as due to convective processes. The implication of the fire plume on the vertical distribution of 0<sub>3</sub> over Kuala Lumpur has been studied. The tropospheric O<sub>3</sub> increased over this location by 10-25 ppbv during Autumn 2006 as compared to Autumn 2005 and 2007. The MOZART model simulation significantly underestimated this tropospheric O<sub>3</sub> enhancement. The model is run both with and without Indonesian biomass burning emissions to estimate the contribution of fire emission in CO and O<sub>3</sub> enhancement. Biomass burning emission is found to be responsible for an average increase in CO by 104 ± 56 ppbv and O<sub>3</sub> by 5 ± 1 ppbv from surface to 100 hPa range. The model results also showed that biomass burning and El Niño related dynamical changes both contributed (∼4 ppbv-12 ppbv) to the observed increase in tropospheric O<sub>3</sub> over the Indonesian region during Autumn 2006.</EA><CC>001D16C02</CC><FD>Troposphère; Ozone; Monoxyde de carbone; Traceur; Feu végétation; Biomasse; Combustion; Transport chimique; Modèle 3 dimensions; Panache; Pollution air; Distribution concentration; Indonésie; Oxydant photochimique</FD><FG>Asie</FG><ED>Troposphere; Ozone; Carbon monoxide; Tracers; Vegetation fire; Biomass; Combustion; Chemical transport; Three dimensional model; Plume; Air pollution; Concentration distribution; Indonesia; Photochemical oxidants</ED><EG>Asia</EG><SD>Troposfera; Ozono; Carbono monóxido; Trazador; Fuego vegetación; Biomasa; Combustión; Transporte químico; Modelo 3 dimensiones; Penacho; Contaminación aire; Distribución concentración; Indonesia</SD><LO>INIST-8940B.354000506371730070</LO><ID>13-0194370</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 000025 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 000025 | 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:13-0194370
|texte= Study of tropospheric CO and O3 enhancement episode over Indonesia during Autumn 2006 using the Model for Ozone and Related chemical Tracers (MOZART-4)
}}
| This area was generated with Dilib version V0.6.20. |  |