Evidence of seasonal enhancement of CO in the upper troposphere over India
Identifieur interne : 000094 ( PascalFrancis/Curation ); précédent : 000093; suivant : 000095Evidence of seasonal enhancement of CO in the upper troposphere over India
Auteurs : S. Fadnavis [Inde] ; P. Buchunde [Inde] ; Sachin D. Ghude [Inde] ; S. H. Kulkarni [Inde] ; G. Beig [Inde]Source :
- International journal of remote sensing : (Print) [ 0143-1161 ] ; 2011.
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.
- Wicri :
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.
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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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<fC03 i1="20" i2="2" l="ENG"><s0>ozone</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Ozono</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Traceur chimique</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>chemical tracers</s0>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Transport</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>transport</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Transporte</s0>
<s5>22</s5>
</fC03>
<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>
</fC03>
<fC03 i1="25" i2="X" l="ENG"><s0>Summer monsoon</s0>
<s5>25</s5>
</fC03>
<fC03 i1="25" i2="X" l="SPA"><s0>Monzón verano</s0>
<s5>25</s5>
</fC03>
<fC03 i1="26" i2="2" l="FRE"><s0>Inde</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="ENG"><s0>India</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="26" i2="2" l="SPA"><s0>India</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Asie</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Asia</s0>
<s2>564</s2>
</fC07>
<fN21><s1>058</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>
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