MozartV1, PascalFrancis, Corpus, bibRecord, 000046

Evidence of seasonal enhancement of CO in the upper troposphere over India

Identifieur interne : 000046 ( PascalFrancis/Corpus ); précédent : 000045; suivant : 000047

Evidence of seasonal enhancement of CO in the upper troposphere over India

Auteurs : S. Fadnavis ; P. Buchunde ; Sachin D. Ghude ; S. H. Kulkarni ; G. Beig

Source :

International journal of remote sensing : (Print) [ 0143-1161 ] ; 2011.

RBID : Pascal:12-0076575

Descripteurs français

Pascal (Inist)
- Variation saisonnière, Troposphère, Profil vertical, Monoxyde carbone, Monoxyde de carbone, Rapport mélange, EOS, Hyperfréquence, Membre, Satellite, 2005, 2009, Spectromètre, 2006, 2007, Evolution, Polluant, Modèle, Modélisation, Ozone, Traceur chimique, Transport, Observation par satellite, Vertical, Mousson été, Inde.

English descriptors

KwdEn :
- 2005, 2006, 2007, 2009, Carbon monoxide, Earth Observing System, India, Limb, Mixing ratio, Modeling, Satellite observation, Spectrometer, Summer monsoon, Vertical, Vertical profile, carbon monoxide, chemical tracers, evolution, microwaves, models, ozone, pollutants, satellites, seasonal variations, transport, troposphere.

Abstract

The vertical profiles of carbon monoxide (CO) mixing ratios retrieved from the Earth Observing System (EOS), Microwave Limb Sounder (MLS) onboard the Aura satellite for the period 2005-2009 and the EOS Tropospheric Emission Spectrometer (TES) onboard Aura for the period 2006-2007 were used to examine the evolution of pollutant CO in the upper troposphere (UT) over India. The Model for OZone And Related chemical Tracers version 2 (MOZART-2) was used to examine the seasonal transport of CO in the UT. The satellite observations revealed vertical transport of CO (80-90 ppb) from the surface to the UT during the summer monsoon season. The regular feature of enhancement of CO in the UT over India is presented. The results obtained by the MOZART-2 simulations (for the years 2000-2005) agree with the observations and indicate transport of boundary layer CO to the tropopause during the monsoon season. The observed enhanced CO mixing ratios in the UT are explained by processes involving monsoon convection.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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Format Inist (serveur)

NO :	PASCAL 12-0076575 INIST
ET :	Evidence of seasonal enhancement of CO in the upper troposphere over India
AU :	FADNAVIS (S.); BUCHUNDE (P.); GHUDE (Sachin D.); KULKARNI (S. H.); BEIG (G.)
AF :	Indian Institute of Tropical Meteorology, Dr. Homi Bhabha Road, Pashan/Pune 411008/Inde (1 aut., 2 aut., 3 aut., 4 aut., 5 aut.)
DT :	Publication en série; Niveau analytique
SO :	International journal of remote sensing : (Print); ISSN 0143-1161; Coden IJSEDK; Royaume-Uni; Da. 2011; Vol. 32; No. 22; Pp. 7441-7452; Bibl. 2 p.
LA :	Anglais
EA :	The vertical profiles of carbon monoxide (CO) mixing ratios retrieved from the Earth Observing System (EOS), Microwave Limb Sounder (MLS) onboard the Aura satellite for the period 2005-2009 and the EOS Tropospheric Emission Spectrometer (TES) onboard Aura for the period 2006-2007 were used to examine the evolution of pollutant CO in the upper troposphere (UT) over India. The Model for OZone And Related chemical Tracers version 2 (MOZART-2) was used to examine the seasonal transport of CO in the UT. The satellite observations revealed vertical transport of CO (80-90 ppb) from the surface to the UT during the summer monsoon season. The regular feature of enhancement of CO in the UT over India is presented. The results obtained by the MOZART-2 simulations (for the years 2000-2005) agree with the observations and indicate transport of boundary layer CO to the tropopause during the monsoon season. The observed enhanced CO mixing ratios in the UT are explained by processes involving monsoon convection.
CC :	002A14A03; 001E01M04; 225B04
FD :	Variation saisonnière; Troposphère; Profil vertical; Monoxyde carbone; Monoxyde de carbone; Rapport mélange; EOS; Hyperfréquence; Membre; Satellite; 2005; 2009; Spectromètre; 2006; 2007; Evolution; Polluant; Modèle; Modélisation; Ozone; Traceur chimique; Transport; Observation par satellite; Vertical; Mousson été; Inde
FG :	Asie
ED :	seasonal variations; troposphere; Vertical profile; carbon monoxide; Carbon monoxide; Mixing ratio; Earth Observing System; microwaves; Limb; satellites; 2005; 2009; Spectrometer; 2006; 2007; evolution; pollutants; models; Modeling; ozone; chemical tracers; transport; Satellite observation; Vertical; Summer monsoon; India
EG :	Asia
SD :	Variación estacional; Perfil vertical; Carbono monóxido; Relación mezcla; Miembro; Satélite; 2005; 2009; Espectrómetro; 2006; 2007; Contaminante; Modelo; Modelización; Ozono; Transporte; Observación por satélite; Vertical; Monzón verano; India
LO :	INIST-19437.354000505580560280
ID :	12-0076575

Links to Exploration step

Pascal:12-0076575

Le document en format XML

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<front><div type="abstract" xml:lang="en">The vertical profiles of carbon monoxide (CO) mixing ratios retrieved from the Earth Observing System (EOS), Microwave Limb Sounder (MLS) onboard the Aura satellite for the period 2005-2009 and the EOS Tropospheric Emission Spectrometer (TES) onboard Aura for the period 2006-2007 were used to examine the evolution of pollutant CO in the upper troposphere (UT) over India. The Model for OZone And Related chemical Tracers version 2 (MOZART-2) was used to examine the seasonal transport of CO in the UT. The satellite observations revealed vertical transport of CO (80-90 ppb) from the surface to the UT during the summer monsoon season. The regular feature of enhancement of CO in the UT over India is presented. The results obtained by the MOZART-2 simulations (for the years 2000-2005) agree with the observations and indicate transport of boundary layer CO to the tropopause during the monsoon season. The observed enhanced CO mixing ratios in the UT are explained by processes involving monsoon convection.</div>
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<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
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<fA20><s1>7441-7452</s1>
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<fA61><s0>A</s0>
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<fA64 i1="01" i2="1"><s0>International journal of remote sensing : (Print)</s0>
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<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>The vertical profiles of carbon monoxide (CO) mixing ratios retrieved from the Earth Observing System (EOS), Microwave Limb Sounder (MLS) onboard the Aura satellite for the period 2005-2009 and the EOS Tropospheric Emission Spectrometer (TES) onboard Aura for the period 2006-2007 were used to examine the evolution of pollutant CO in the upper troposphere (UT) over India. The Model for OZone And Related chemical Tracers version 2 (MOZART-2) was used to examine the seasonal transport of CO in the UT. The satellite observations revealed vertical transport of CO (80-90 ppb) from the surface to the UT during the summer monsoon season. The regular feature of enhancement of CO in the UT over India is presented. The results obtained by the MOZART-2 simulations (for the years 2000-2005) agree with the observations and indicate transport of boundary layer CO to the tropopause during the monsoon season. The observed enhanced CO mixing ratios in the UT are explained by processes involving monsoon convection.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>002A14A03</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01M04</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>225B04</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Variation saisonnière</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>seasonal variations</s0>
<s5>01</s5>
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<s5>02</s5>
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<fC03 i1="02" i2="2" l="ENG"><s0>troposphere</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Profil vertical</s0>
<s5>03</s5>
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<fC03 i1="03" i2="X" l="ENG"><s0>Vertical profile</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Perfil vertical</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Monoxyde carbone</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>carbon monoxide</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Monoxyde de carbone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Carbon monoxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Carbono monóxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Rapport mélange</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Mixing ratio</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Relación mezcla</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>EOS</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>Earth Observing System</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Hyperfréquence</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>microwaves</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Membre</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Limb</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Miembro</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Satellite</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>satellites</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Satélite</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>2005</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>2005</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>2005</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>2009</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>2009</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>2009</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Spectromètre</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Spectrometer</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Espectrómetro</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>2006</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>2006</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>2006</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>2007</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>2007</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>2007</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Evolution</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>evolution</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Polluant</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>pollutants</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Contaminante</s0>
<s5>17</s5>
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<fC03 i1="18" i2="2" l="FRE"><s0>Modèle</s0>
<s5>18</s5>
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<fC03 i1="18" i2="2" l="ENG"><s0>models</s0>
<s5>18</s5>
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<fC03 i1="18" i2="2" l="SPA"><s0>Modelo</s0>
<s5>18</s5>
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<s5>19</s5>
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<s5>19</s5>
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<s5>19</s5>
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<s5>20</s5>
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<fC03 i1="20" i2="2" l="ENG"><s0>ozone</s0>
<s5>20</s5>
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<fC03 i1="20" i2="2" l="SPA"><s0>Ozono</s0>
<s5>20</s5>
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<fC03 i1="21" i2="2" l="FRE"><s0>Traceur chimique</s0>
<s5>21</s5>
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<fC03 i1="21" i2="2" l="ENG"><s0>chemical tracers</s0>
<s5>21</s5>
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<fC03 i1="22" i2="2" l="FRE"><s0>Transport</s0>
<s5>22</s5>
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<fC03 i1="22" i2="2" l="ENG"><s0>transport</s0>
<s5>22</s5>
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<fC03 i1="22" i2="2" l="SPA"><s0>Transporte</s0>
<s5>22</s5>
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<fC03 i1="23" i2="X" l="FRE"><s0>Observation par satellite</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="X" l="ENG"><s0>Satellite observation</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="X" l="SPA"><s0>Observación por satélite</s0>
<s5>23</s5>
</fC03>
<fC03 i1="24" i2="X" l="FRE"><s0>Vertical</s0>
<s5>24</s5>
</fC03>
<fC03 i1="24" i2="X" l="ENG"><s0>Vertical</s0>
<s5>24</s5>
</fC03>
<fC03 i1="24" i2="X" l="SPA"><s0>Vertical</s0>
<s5>24</s5>
</fC03>
<fC03 i1="25" i2="X" l="FRE"><s0>Mousson été</s0>
<s5>25</s5>
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<fC03 i1="25" i2="X" l="ENG"><s0>Summer monsoon</s0>
<s5>25</s5>
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<fC03 i1="25" i2="X" l="SPA"><s0>Monzón verano</s0>
<s5>25</s5>
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<fC03 i1="26" i2="2" l="FRE"><s0>Inde</s0>
<s2>NG</s2>
<s5>61</s5>
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<fC03 i1="26" i2="2" l="ENG"><s0>India</s0>
<s2>NG</s2>
<s5>61</s5>
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<fC03 i1="26" i2="2" l="SPA"><s0>India</s0>
<s2>NG</s2>
<s5>61</s5>
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<fC07 i1="01" i2="2" l="FRE"><s0>Asie</s0>
<s2>564</s2>
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<s2>564</s2>
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<fC07 i1="01" i2="2" l="SPA"><s0>Asia</s0>
<s2>564</s2>
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<fN21><s1>058</s1>
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<fN44 i1="01"><s1>OTO</s1>
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<fN82><s1>OTO</s1>
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<server><NO>PASCAL 12-0076575 INIST</NO>
<ET>Evidence of seasonal enhancement of CO in the upper troposphere over India</ET>
<AU>FADNAVIS (S.); BUCHUNDE (P.); GHUDE (Sachin D.); KULKARNI (S. H.); BEIG (G.)</AU>
<AF>Indian Institute of Tropical Meteorology, Dr. Homi Bhabha Road, Pashan/Pune 411008/Inde (1 aut., 2 aut., 3 aut., 4 aut., 5 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>International journal of remote sensing : (Print); ISSN 0143-1161; Coden IJSEDK; Royaume-Uni; Da. 2011; Vol. 32; No. 22; Pp. 7441-7452; Bibl. 2 p.</SO>
<LA>Anglais</LA>
<EA>The vertical profiles of carbon monoxide (CO) mixing ratios retrieved from the Earth Observing System (EOS), Microwave Limb Sounder (MLS) onboard the Aura satellite for the period 2005-2009 and the EOS Tropospheric Emission Spectrometer (TES) onboard Aura for the period 2006-2007 were used to examine the evolution of pollutant CO in the upper troposphere (UT) over India. The Model for OZone And Related chemical Tracers version 2 (MOZART-2) was used to examine the seasonal transport of CO in the UT. The satellite observations revealed vertical transport of CO (80-90 ppb) from the surface to the UT during the summer monsoon season. The regular feature of enhancement of CO in the UT over India is presented. The results obtained by the MOZART-2 simulations (for the years 2000-2005) agree with the observations and indicate transport of boundary layer CO to the tropopause during the monsoon season. The observed enhanced CO mixing ratios in the UT are explained by processes involving monsoon convection.</EA>
<CC>002A14A03; 001E01M04; 225B04</CC>
<FD>Variation saisonnière; Troposphère; Profil vertical; Monoxyde carbone; Monoxyde de carbone; Rapport mélange; EOS; Hyperfréquence; Membre; Satellite; 2005; 2009; Spectromètre; 2006; 2007; Evolution; Polluant; Modèle; Modélisation; Ozone; Traceur chimique; Transport; Observation par satellite; Vertical; Mousson été; Inde</FD>
<FG>Asie</FG>
<ED>seasonal variations; troposphere; Vertical profile; carbon monoxide; Carbon monoxide; Mixing ratio; Earth Observing System; microwaves; Limb; satellites; 2005; 2009; Spectrometer; 2006; 2007; evolution; pollutants; models; Modeling; ozone; chemical tracers; transport; Satellite observation; Vertical; Summer monsoon; India</ED>
<EG>Asia</EG>
<SD>Variación estacional; Perfil vertical; Carbono monóxido; Relación mezcla; Miembro; Satélite; 2005; 2009; Espectrómetro; 2006; 2007; Contaminante; Modelo; Modelización; Ozono; Transporte; Observación por satélite; Vertical; Monzón verano; India</SD>
<LO>INIST-19437.354000505580560280</LO>
<ID>12-0076575</ID>
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Evidence of seasonal enhancement of CO in the upper troposphere over India

Evidence of seasonal enhancement of CO in the upper troposphere over India

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