MozartV1, PascalFrancis, Corpus, bibRecord, 000009

Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study

Identifieur interne : 000009 ( PascalFrancis/Corpus ); précédent : 000008; suivant : 000010

Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study

Auteurs : Lieven Clarisse ; Michael Fromm ; Yasmine Ngadi ; Louisa Emmons ; Cathy Clerbaux ; Daniel Hurtmans ; Pierre-François Coheur

Source :

Geophysical research letters [ 0094-8276 ] ; 2011.

RBID : Pascal:14-0045125

Descripteurs français

Pascal (Inist)
- Transport, Facteur anthropique, Dioxyde soufre, Dioxyde de soufre, Polluant, Télédétection spatiale, Etude cas, Surrection, Panache, Trajectoire, Amérique du Nord, Composé trace, Pan, Méthanol, Modèle, Corrélation, Observation par satellite, Chine.

English descriptors

KwdEn :
- Anthropogenic factor, China, Methanol, North America, Pan, Satellite observation, Space remote sensing, Sulfur dioxide, Trace compound, case studies, correlation, models, plumes, pollutants, sulfur dioxide, trajectory, transport, uplifts.

Abstract

[1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO₂, CO, PAN, CH₃OH, HCOOH and C₂H₂). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A11	`02`	`1`		`@1 FROMM (Michael)`
A11	`03`	`1`		`@1 NGADI (Yasmine)`
A11	`04`	`1`		`@1 EMMONS (Louisa)`
A11	`05`	`1`		`@1 CLERBAUX (Cathy)`
A11	`06`	`1`		`@1 HURTMANS (Daniel)`
A11	`07`	`1`		`@1 COHEUR (Pierre-François)`
A14	`01`			`@1 Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles @2 Brussels @3 BEL @Z 1 aut. @Z 3 aut. @Z 5 aut. @Z 6 aut. @Z 7 aut.`
A14	`02`			`@1 U.S. Naval Research Laboratory @2 Washington, DC @3 USA @Z 2 aut.`
A14	`03`			`@1 National Center for Atmospheric Research @2 Boulder, Colorado @3 USA @Z 4 aut.`
A14	`04`			`@1 UPMC Université Paris 6, Université Versailles St.-Quentin, CNRS/INSU, LATMOS-IPSL @2 Paris @3 FRA @Z 5 aut.`
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A44				`@0 0000 @1 © 2014 INIST-CNRS. All rights reserved.`
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C01	`01`		`ENG`	@0 [1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO₂, CO, PAN, CH₃OH, HCOOH and C₂H₂). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.
C02	`01`	`3`		`@0 001E`
C02	`02`	`2`		`@0 001E01`
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C03	`01`	`2`	`FRE`	`@0 Transport @5 01`
C03	`01`	`2`	`ENG`	`@0 transport @5 01`
C03	`01`	`2`	`SPA`	`@0 Transporte @5 01`
C03	`02`	`X`	`FRE`	`@0 Facteur anthropique @5 02`
C03	`02`	`X`	`ENG`	`@0 Anthropogenic factor @5 02`
C03	`02`	`X`	`SPA`	`@0 Factor antrópico @5 02`
C03	`03`	`2`	`FRE`	`@0 Dioxyde soufre @5 03`
C03	`03`	`2`	`ENG`	`@0 sulfur dioxide @5 03`
C03	`04`	`X`	`FRE`	`@0 Dioxyde de soufre @2 NK @2 FX @5 04`
C03	`04`	`X`	`ENG`	`@0 Sulfur dioxide @2 NK @2 FX @5 04`
C03	`04`	`X`	`SPA`	`@0 Dióxido sulfúrico @2 NK @2 FX @5 04`
C03	`05`	`2`	`FRE`	`@0 Polluant @5 05`
C03	`05`	`2`	`ENG`	`@0 pollutants @5 05`
C03	`05`	`2`	`SPA`	`@0 Contaminante @5 05`
C03	`06`	`2`	`FRE`	`@0 Télédétection spatiale @5 06`
C03	`06`	`2`	`ENG`	`@0 Space remote sensing @5 06`
C03	`06`	`2`	`SPA`	`@0 Teledetección espacial @5 06`
C03	`07`	`2`	`FRE`	`@0 Etude cas @5 07`
C03	`07`	`2`	`ENG`	`@0 case studies @5 07`
C03	`07`	`2`	`SPA`	`@0 Estudio caso @5 07`
C03	`08`	`2`	`FRE`	`@0 Surrection @5 08`
C03	`08`	`2`	`ENG`	`@0 uplifts @5 08`
C03	`09`	`2`	`FRE`	`@0 Panache @5 09`
C03	`09`	`2`	`ENG`	`@0 plumes @5 09`
C03	`09`	`2`	`SPA`	`@0 Penacho @5 09`
C03	`10`	`2`	`FRE`	`@0 Trajectoire @5 10`
C03	`10`	`2`	`ENG`	`@0 trajectory @5 10`
C03	`11`	`2`	`FRE`	`@0 Amérique du Nord @5 11`
C03	`11`	`2`	`ENG`	`@0 North America @5 11`
C03	`11`	`2`	`SPA`	`@0 America del norte @5 11`
C03	`12`	`X`	`FRE`	`@0 Composé trace @5 12`
C03	`12`	`X`	`ENG`	`@0 Trace compound @5 12`
C03	`12`	`X`	`SPA`	`@0 Compuesto huella @5 12`
C03	`13`	`X`	`FRE`	`@0 Pan @2 NO @5 13`
C03	`13`	`X`	`ENG`	`@0 Pan @2 NO @5 13`
C03	`13`	`X`	`SPA`	`@0 Pan @2 NO @5 13`
C03	`14`	`X`	`FRE`	`@0 Méthanol @2 NK @2 FX @5 14`
C03	`14`	`X`	`ENG`	`@0 Methanol @2 NK @2 FX @5 14`
C03	`14`	`X`	`SPA`	`@0 Metanol @2 NK @2 FX @5 14`
C03	`15`	`2`	`FRE`	`@0 Modèle @5 15`
C03	`15`	`2`	`ENG`	`@0 models @5 15`
C03	`15`	`2`	`SPA`	`@0 Modelo @5 15`
C03	`16`	`2`	`FRE`	`@0 Corrélation @5 16`
C03	`16`	`2`	`ENG`	`@0 correlation @5 16`
C03	`16`	`2`	`SPA`	`@0 Correlación @5 16`
C03	`17`	`X`	`FRE`	`@0 Observation par satellite @5 17`
C03	`17`	`X`	`ENG`	`@0 Satellite observation @5 17`
C03	`17`	`X`	`SPA`	`@0 Observación por satélite @5 17`
C03	`18`	`2`	`FRE`	`@0 Chine @2 NG @5 61`
C03	`18`	`2`	`ENG`	`@0 China @2 NG @5 61`
C03	`18`	`2`	`SPA`	`@0 China @2 NG @5 61`
C07	`01`	`2`	`FRE`	`@0 Extrême Orient @2 NG`
C07	`01`	`2`	`ENG`	`@0 Far East @2 NG`
C07	`01`	`2`	`SPA`	`@0 Extremo Oriente @2 NG`
C07	`02`	`2`	`FRE`	`@0 Asie @2 564`
C07	`02`	`2`	`ENG`	`@0 Asia @2 564`
C07	`02`	`2`	`SPA`	`@0 Asia @2 564`
N21				`@1 055`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

Format Inist (serveur)

NO :	PASCAL 14-0045125 INIST
ET :	Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study
AU :	CLARISSE (Lieven); FROMM (Michael); NGADI (Yasmine); EMMONS (Louisa); CLERBAUX (Cathy); HURTMANS (Daniel); COHEUR (Pierre-François)
AF :	Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles/Brussels/Belgique (1 aut., 3 aut., 5 aut., 6 aut., 7 aut.); U.S. Naval Research Laboratory/Washington, DC/Etats-Unis (2 aut.); National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (4 aut.); UPMC Université Paris 6, Université Versailles St.-Quentin, CNRS/INSU, LATMOS-IPSL/Paris/France (5 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2011; Vol. 38; No. 19; L19806.1-L19806.5; Bibl. 3/4 p.
LA :	Anglais
EA :	[1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO₂, CO, PAN, CH₃OH, HCOOH and C₂H₂). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.
CC :	001E; 001E01; 220
FD :	Transport; Facteur anthropique; Dioxyde soufre; Dioxyde de soufre; Polluant; Télédétection spatiale; Etude cas; Surrection; Panache; Trajectoire; Amérique du Nord; Composé trace; Pan; Méthanol; Modèle; Corrélation; Observation par satellite; Chine
FG :	Extrême Orient; Asie
ED :	transport; Anthropogenic factor; sulfur dioxide; Sulfur dioxide; pollutants; Space remote sensing; case studies; uplifts; plumes; trajectory; North America; Trace compound; Pan; Methanol; models; correlation; Satellite observation; China
EG :	Far East; Asia
SD :	Transporte; Factor antrópico; Dióxido sulfúrico; Contaminante; Teledetección espacial; Estudio caso; Penacho; America del norte; Compuesto huella; Pan; Metanol; Modelo; Correlación; Observación por satélite; China
LO :	INIST-16687.354000501660740490
ID :	14-0045125

Links to Exploration step

Pascal:14-0045125

Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Anthropogenic factor</term>
<term>China</term>
<term>Methanol</term>
<term>North America</term>
<term>Pan</term>
<term>Satellite observation</term>
<term>Space remote sensing</term>
<term>Sulfur dioxide</term>
<term>Trace compound</term>
<term>case studies</term>
<term>correlation</term>
<term>models</term>
<term>plumes</term>
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<term>sulfur dioxide</term>
<term>trajectory</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Transport</term>
<term>Facteur anthropique</term>
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<term>Télédétection spatiale</term>
<term>Etude cas</term>
<term>Surrection</term>
<term>Panache</term>
<term>Trajectoire</term>
<term>Amérique du Nord</term>
<term>Composé trace</term>
<term>Pan</term>
<term>Méthanol</term>
<term>Modèle</term>
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<term>Observation par satellite</term>
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<front><div type="abstract" xml:lang="en">[1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO<sub>2</sub>
, CO, PAN, CH<sub>3</sub>
OH, HCOOH and C<sub>2</sub>
H<sub>2</sub>
). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.</div>
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<fA03 i2="1"><s0>Geophys. res. lett.</s0>
</fA03>
<fA05><s2>38</s2>
</fA05>
<fA06><s2>19</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>CLARISSE (Lieven)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>FROMM (Michael)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>NGADI (Yasmine)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>EMMONS (Louisa)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>CLERBAUX (Cathy)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>HURTMANS (Daniel)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>COHEUR (Pierre-François)</s1>
</fA11>
<fA14 i1="01"><s1>Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles</s1>
<s2>Brussels</s2>
<s3>BEL</s3>
<sZ>1 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>U.S. Naval Research Laboratory</s1>
<s2>Washington, DC</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>UPMC Université Paris 6, Université Versailles St.-Quentin, CNRS/INSU, LATMOS-IPSL</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA20><s2>L19806.1-L19806.5</s2>
</fA20>
<fA21><s1>2011</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>16687</s2>
<s5>354000501660740490</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2014 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3/4 p.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>14-0045125</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Geophysical research letters</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>[1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO<sub>2</sub>
, CO, PAN, CH<sub>3</sub>
OH, HCOOH and C<sub>2</sub>
H<sub>2</sub>
). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.</s0>
</fC01>
<fC02 i1="01" i2="3"><s0>001E</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>220</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Transport</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>transport</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Transporte</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Facteur anthropique</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Anthropogenic factor</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Factor antrópico</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Dioxyde soufre</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>sulfur dioxide</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Dioxyde de soufre</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Sulfur dioxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Dióxido sulfúrico</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Polluant</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>pollutants</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Contaminante</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Télédétection spatiale</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>Space remote sensing</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Teledetección espacial</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Etude cas</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>case studies</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Estudio caso</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Surrection</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>uplifts</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Panache</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>plumes</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Penacho</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Trajectoire</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>trajectory</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Amérique du Nord</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>North America</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>America del norte</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Composé trace</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Trace compound</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Compuesto huella</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Pan</s0>
<s2>NO</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Pan</s0>
<s2>NO</s2>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Pan</s0>
<s2>NO</s2>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Méthanol</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Methanol</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Metanol</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Modèle</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>models</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Modelo</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Corrélation</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>correlation</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Correlación</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="X" l="FRE"><s0>Observation par satellite</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="ENG"><s0>Satellite observation</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="X" l="SPA"><s0>Observación por satélite</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Chine</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>China</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>China</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Extrême Orient</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Far East</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Extremo Oriente</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Asie</s0>
<s2>564</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fN21><s1>055</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 14-0045125 INIST</NO>
<ET>Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study</ET>
<AU>CLARISSE (Lieven); FROMM (Michael); NGADI (Yasmine); EMMONS (Louisa); CLERBAUX (Cathy); HURTMANS (Daniel); COHEUR (Pierre-François)</AU>
<AF>Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles/Brussels/Belgique (1 aut., 3 aut., 5 aut., 6 aut., 7 aut.); U.S. Naval Research Laboratory/Washington, DC/Etats-Unis (2 aut.); National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (4 aut.); UPMC Université Paris 6, Université Versailles St.-Quentin, CNRS/INSU, LATMOS-IPSL/Paris/France (5 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geophysical research letters; ISSN 0094-8276; Coden GPRLAJ; Etats-Unis; Da. 2011; Vol. 38; No. 19; L19806.1-L19806.5; Bibl. 3/4 p.</SO>
<LA>Anglais</LA>
<EA>[1] Using 3 years worth of IASI (the Infrared Atmospheric Sounder Interferometer aboard METOP-A) measurements, we have identified 24 major events of uplift and transport of anthropogenic sulfur dioxide. These were all first observed over East Asia, and could be traced for over 60 hours. On 7 November 2010 a sulfur dioxide plume was observed over Northeast China and tracked for five days to North America. We discuss this event in detail with respect to build up; uplift and in-plume chemistry. We found a host of trace gas enhancements in the plume (SO<sub>2</sub>
, CO, PAN, CH<sub>3</sub>
OH, HCOOH and C<sub>2</sub>
H<sub>2</sub>
). A reasonable to very good agreement was found with MOZART-4 modeled ambient columns for all species except methanol, which was underestimated by the model by an order of magnitude. We calculate correlations of the different species and give observational evidence of secondary in-plume formation of methanol and PAN.</EA>
<CC>001E; 001E01; 220</CC>
<FD>Transport; Facteur anthropique; Dioxyde soufre; Dioxyde de soufre; Polluant; Télédétection spatiale; Etude cas; Surrection; Panache; Trajectoire; Amérique du Nord; Composé trace; Pan; Méthanol; Modèle; Corrélation; Observation par satellite; Chine</FD>
<FG>Extrême Orient; Asie</FG>
<ED>transport; Anthropogenic factor; sulfur dioxide; Sulfur dioxide; pollutants; Space remote sensing; case studies; uplifts; plumes; trajectory; North America; Trace compound; Pan; Methanol; models; correlation; Satellite observation; China</ED>
<EG>Far East; Asia</EG>
<SD>Transporte; Factor antrópico; Dióxido sulfúrico; Contaminante; Teledetección espacial; Estudio caso; Penacho; America del norte; Compuesto huella; Pan; Metanol; Modelo; Correlación; Observación por satélite; China</SD>
<LO>INIST-16687.354000501660740490</LO>
<ID>14-0045125</ID>
</server>
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Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study

Intercontinental transport of anthropogenic sulfur dioxide and other pollutants: An infrared remote sensing case study

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