MozartV1, PascalFrancis, Corpus, bibRecord, 000150

Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)

Identifieur interne : 000150 ( PascalFrancis/Corpus ); précédent : 000149; suivant : 000151

Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)

Auteurs : D. P. Edwards ; G. Petron ; P. C. Novelli ; L. K. Emmons ; J. C. Gille ; J. R. Drummond

Source :

Journal of geophysical research [ 0148-0227 ] ; 2006.

RBID : Pascal:06-0463930

Descripteurs français

Pascal (Inist)
- Hémisphère Sud, Monoxyde carbone, Carbone monoxyde, Variation interannuelle, Pollution, Troposphère, Feu végétation, Echelon régional, Durée vie, Traceur, Transport, Composé trace, Satellite, Long terme, Monde, Instrumentation, Chargement, Climat, Intensité, Incendie, Printemps, Saison sèche, Amérique du Sud, Continent, El Nino, Afrique du Sud, Afrique australe, Australie, Asie Sud Est.

English descriptors

KwdEn :
- Australia, Carbon monoxide, Dry season, El Nino, Interannual variation, Lifetime, Long term, Regional scope, South America, Southeast Asia, Southern Africa, Southern Hemisphere, Spring(season), Trace compound, Vegetation fire, carbon monoxide, climate, continents, fires, global, instruments, intensity, loading, pollution, satellites, tracers, transport, troposphere.

Abstract

[1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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C01	`01`		`ENG`	@0 [1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.
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C03	`14`	`X`	`SPA`	`@0 Largo plazo @5 14`
C03	`15`	`2`	`FRE`	`@0 Monde @5 15`
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C03	`15`	`2`	`SPA`	`@0 Mundo @5 15`
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C03	`18`	`2`	`ENG`	`@0 climate @5 18`
C03	`18`	`2`	`SPA`	`@0 Clima @5 18`
C03	`19`	`2`	`FRE`	`@0 Intensité @5 19`
C03	`19`	`2`	`ENG`	`@0 intensity @5 19`
C03	`19`	`2`	`SPA`	`@0 Intensidad @5 19`
C03	`20`	`2`	`FRE`	`@0 Incendie @5 20`
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Format Inist (serveur)

NO :	PASCAL 06-0463930 INIST
ET :	Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)
AU :	EDWARDS (D. P.); PETRON (G.); NOVELLI (P. C.); EMMONS (L. K.); GILLE (J. C.); DRUMMOND (J. R.)
AF :	National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 4 aut., 5 aut.); Earth System Research Laboratory, Global Monitoring Division, NOAA/Boulder, Colorado/Etats-Unis (2 aut., 3 aut.); Department of Physics, University of Toronto/Toronto, Ontario/Canada (6 aut.)
DT :	Publication en série; Niveau analytique
SO :	Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2006; Vol. 111; No. D16; D16303.1-D16303.9; Bibl. 35 ref.
LA :	Anglais
EA :	[1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.
CC :	220; 001E; 001E01
FD :	Hémisphère Sud; Monoxyde carbone; Carbone monoxyde; Variation interannuelle; Pollution; Troposphère; Feu végétation; Echelon régional; Durée vie; Traceur; Transport; Composé trace; Satellite; Long terme; Monde; Instrumentation; Chargement; Climat; Intensité; Incendie; Printemps; Saison sèche; Amérique du Sud; Continent; El Nino; Afrique du Sud; Afrique australe; Australie; Asie Sud Est
FG :	Afrique; Afrique; Australasie; Asie
ED :	Southern Hemisphere; carbon monoxide; Carbon monoxide; Interannual variation; pollution; troposphere; Vegetation fire; Regional scope; Lifetime; tracers; transport; Trace compound; satellites; Long term; global; instruments; loading; climate; intensity; fires; Spring(season); Dry season; South America; continents; El Nino; Southern Africa; Southern Africa; Australia; Southeast Asia
EG :	Africa; Africa; Australasia; Asia
SD :	Hemisferio sur; Carbono monóxido; Variación interanual; Polución; Fuego vegetación; Escala regional; Tiempo vida; Trazador; Transporte; Compuesto huella; Satélite; Largo plazo; Mundo; Instrumentación; Cargamento; Clima; Intensidad; Primavera; Estación seca; America del sur; África Sur; Africa austral; Australia
LO :	INIST-3144.354000157227140260
ID :	06-0463930

Links to Exploration step

Pascal:06-0463930

Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Australia</term>
<term>Carbon monoxide</term>
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<term>El Nino</term>
<term>Interannual variation</term>
<term>Lifetime</term>
<term>Long term</term>
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<term>Southeast Asia</term>
<term>Southern Africa</term>
<term>Southern Hemisphere</term>
<term>Spring(season)</term>
<term>Trace compound</term>
<term>Vegetation fire</term>
<term>carbon monoxide</term>
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<term>global</term>
<term>instruments</term>
<term>intensity</term>
<term>loading</term>
<term>pollution</term>
<term>satellites</term>
<term>tracers</term>
<term>transport</term>
<term>troposphere</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Hémisphère Sud</term>
<term>Monoxyde carbone</term>
<term>Carbone monoxyde</term>
<term>Variation interannuelle</term>
<term>Pollution</term>
<term>Troposphère</term>
<term>Feu végétation</term>
<term>Echelon régional</term>
<term>Durée vie</term>
<term>Traceur</term>
<term>Transport</term>
<term>Composé trace</term>
<term>Satellite</term>
<term>Long terme</term>
<term>Monde</term>
<term>Instrumentation</term>
<term>Chargement</term>
<term>Climat</term>
<term>Intensité</term>
<term>Incendie</term>
<term>Printemps</term>
<term>Saison sèche</term>
<term>Amérique du Sud</term>
<term>Continent</term>
<term>El Nino</term>
<term>Afrique du Sud</term>
<term>Afrique australe</term>
<term>Australie</term>
<term>Asie Sud Est</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">[1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.</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>111</s2>
</fA05>
<fA06><s2>D16</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>EDWARDS (D. P.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>PETRON (G.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>NOVELLI (P. C.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>EMMONS (L. K.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>GILLE (J. C.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>DRUMMOND (J. R.)</s1>
</fA11>
<fA14 i1="01"><s1>National Center for Atmospheric Research</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>1 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Earth System Research Laboratory, Global Monitoring Division, NOAA</s1>
<s2>Boulder, Colorado</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Department of Physics, University of Toronto</s1>
<s2>Toronto, Ontario</s2>
<s3>CAN</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA20><s2>D16303.1-D16303.9</s2>
</fA20>
<fA21><s1>2006</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>3144</s2>
<s5>354000157227140260</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2006 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>35 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>06-0463930</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of geophysical research</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>[1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>220</s0>
</fC02>
<fC02 i1="02" i2="3"><s0>001E</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Hémisphère Sud</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>Southern Hemisphere</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Hemisferio sur</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Monoxyde carbone</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>carbon monoxide</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Carbone monoxyde</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>Variation interannuelle</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Interannual variation</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Variación interanual</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Pollution</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>pollution</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Polución</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Troposphère</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>troposphere</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Feu végétation</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Vegetation fire</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Fuego vegetación</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Echelon régional</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Regional scope</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Escala regional</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Durée vie</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Lifetime</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Tiempo vida</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Traceur</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>tracers</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Trazador</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Transport</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>transport</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Transporte</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="2" l="FRE"><s0>Satellite</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>satellites</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Satélite</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Long terme</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Long term</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Largo plazo</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Monde</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>global</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Mundo</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Instrumentation</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>instruments</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Instrumentación</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Chargement</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>loading</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Cargamento</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Climat</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>climate</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Clima</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Intensité</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>intensity</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Intensidad</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Incendie</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>fires</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="X" l="FRE"><s0>Printemps</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="ENG"><s0>Spring(season)</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="X" l="SPA"><s0>Primavera</s0>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="X" l="FRE"><s0>Saison sèche</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="X" l="ENG"><s0>Dry season</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="X" l="SPA"><s0>Estación seca</s0>
<s5>22</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Amérique du Sud</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>South America</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>America del sur</s0>
<s5>23</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Continent</s0>
<s5>24</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>continents</s0>
<s5>24</s5>
</fC03>
<fC03 i1="25" i2="2" l="FRE"><s0>El Nino</s0>
<s5>25</s5>
</fC03>
<fC03 i1="25" i2="2" l="ENG"><s0>El Nino</s0>
<s5>25</s5>
</fC03>
<fC03 i1="26" i2="2" l="FRE"><s0>Afrique du Sud</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="ENG"><s0>Southern Africa</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="SPA"><s0>África Sur</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="27" i2="X" l="FRE"><s0>Afrique australe</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="27" i2="X" l="ENG"><s0>Southern Africa</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="27" i2="X" l="SPA"><s0>Africa austral</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="28" i2="2" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>63</s5>
</fC03>
<fC03 i1="28" i2="2" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>63</s5>
</fC03>
<fC03 i1="28" i2="2" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>63</s5>
</fC03>
<fC03 i1="29" i2="2" l="FRE"><s0>Asie Sud Est</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="29" i2="2" l="ENG"><s0>Southeast Asia</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Afrique</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Africa</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Africa</s0>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Afrique</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Africa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Africa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Asie</s0>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Asia</s0>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Asia</s0>
</fC07>
<fN21><s1>303</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 06-0463930 INIST</NO>
<ET>Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)</ET>
<AU>EDWARDS (D. P.); PETRON (G.); NOVELLI (P. C.); EMMONS (L. K.); GILLE (J. C.); DRUMMOND (J. R.)</AU>
<AF>National Center for Atmospheric Research/Boulder, Colorado/Etats-Unis (1 aut., 4 aut., 5 aut.); Earth System Research Laboratory, Global Monitoring Division, NOAA/Boulder, Colorado/Etats-Unis (2 aut., 3 aut.); Department of Physics, University of Toronto/Toronto, Ontario/Canada (6 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2006; Vol. 111; No. D16; D16303.1-D16303.9; Bibl. 35 ref.</SO>
<LA>Anglais</LA>
<EA>[1] Biomass burning is an annual occurrence in the tropical Southern Hemisphere (SH) and represents a major source of regional pollution. Vegetation fires emit carbon monoxide (CO), which because of its medium lifetime is an excellent tracer of tropospheric transport. CO is also one of the few tropospheric trace gases currently observed from satellite, and this provides long-term global measurements. In this paper, we use the 5-year CO data record from the Measurement of Pollution in the Troposphere (MOPITT) instrument to examine the interannual variability of the SH CO loading and show how this relates to climate conditions which determine the intensity of fire sources. The MOPITT observations show an annual austral springtime peak in the SH zonal CO loading each year with dry season biomass burning emissions in South America, southern Africa, the maritime continent, and northwestern Australia. Although fires in southern Africa and South America typically produce the greatest amount of CO, the most significant interannual variation is due to varying fire activity and emissions from the maritime continent and northern Australia. We find that this variation in turn correlates well with the El Nino-Southern Oscillation precipitation index. Between 2000 and 2005, emissions were greatest in late 2002, and an inverse modeling of the MOPITT data using the Model of Ozone Research in the Troposphere (MOZART) chemical transport model estimates the Southeast Asia regional fire source for the year August 2002 to September 2003 to be 52 Tg CO. Comparison of the MOPITT retrievals and NOAA surface network measurements indicate that the latter do not fully capture the interannual variability or the seasonal range of the CO zonal average concentration because of biases associated with atmospheric and geographic sampling.</EA>
<CC>220; 001E; 001E01</CC>
<FD>Hémisphère Sud; Monoxyde carbone; Carbone monoxyde; Variation interannuelle; Pollution; Troposphère; Feu végétation; Echelon régional; Durée vie; Traceur; Transport; Composé trace; Satellite; Long terme; Monde; Instrumentation; Chargement; Climat; Intensité; Incendie; Printemps; Saison sèche; Amérique du Sud; Continent; El Nino; Afrique du Sud; Afrique australe; Australie; Asie Sud Est</FD>
<FG>Afrique; Afrique; Australasie; Asie</FG>
<ED>Southern Hemisphere; carbon monoxide; Carbon monoxide; Interannual variation; pollution; troposphere; Vegetation fire; Regional scope; Lifetime; tracers; transport; Trace compound; satellites; Long term; global; instruments; loading; climate; intensity; fires; Spring(season); Dry season; South America; continents; El Nino; Southern Africa; Southern Africa; Australia; Southeast Asia</ED>
<EG>Africa; Africa; Australasia; Asia</EG>
<SD>Hemisferio sur; Carbono monóxido; Variación interanual; Polución; Fuego vegetación; Escala regional; Tiempo vida; Trazador; Transporte; Compuesto huella; Satélite; Largo plazo; Mundo; Instrumentación; Cargamento; Clima; Intensidad; Primavera; Estación seca; America del sur; África Sur; Africa austral; Australia</SD>
<LO>INIST-3144.354000157227140260</LO>
<ID>06-0463930</ID>
</server>
</inist>
</record>

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   |wiki=    Wicri/Musique
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   |flux=    PascalFrancis
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   |clé=     Pascal:06-0463930
   |texte=   Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)
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Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)

Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)

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Abstract

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