MozartV1, PascalFrancis, Curation, bibRecord, 000081

Seasonal stratospheric intrusion of ozone in the upper troposphere over India

Identifieur interne : 000081 ( PascalFrancis/Curation ); précédent : 000080; suivant : 000082

Seasonal stratospheric intrusion of ozone in the upper troposphere over India

Auteurs : S. Fadnavis [Inde] ; T. Chakraborty [Inde] ; G. Beig [Inde]

Source :

Annales geophysicae : (1988) [ 0992-7689 ] ; 2010.

RBID : Pascal:11-0033990

Descripteurs français

Pascal (Inist)
- Stratosphère, Ozone, Troposphère, Inde, Modèle, Traceur, Répartition altitudinale, Rapport mélange, Observation par satellite, Mousson hiver, Tourbillon potentiel, Tropopause, Humidité relative, Corrélation, Structure atmosphérique, Composition atmosphérique, Télédétection spatiale, Sondeur du limbe en hyperfréquence.
Wicri :
- geographic : Inde.
- topic : Ozone.

English descriptors

KwdEn :
- Altitudinal distribution, Atmospheric composition, Atmospheric structure, India, Microwave limb sounder, Mixing ratio, Potential vorticity, Relative humidity, Satellite observation, Space remote sensing, Tropopause, Winter monsoon, correlation, models, ozone, stratosphere, tracers, troposphere.

Abstract

The Model for Ozone and Related chemical Tracers-2 (MOZART-2) is used to examine the evolution of pollutant O₃ in the upper troposphere over the Indian region. Vertical profiles of ozone mixing ratio retrieved from Microwave Limb Sounder (MLS) aboard Earth Observing System (EOS) AURA satellite for the period 2005-2009 and Tropospheric Emission Spectrometer (TES) aboard (EOS) AURA for the period 2006-2007 has been analyzed. The satellite observations reveal the evidence of downward propagation of ozone (100-200 ppb) due to stratospheric intrusion during the winter and pre-monsoon seasons. The regular feature of enhancement of ozone in the upper troposphere over India is presented. Results obtained by the MOZART-2 simulations (for years 2000-2005) confirm the observations and indicate stratospheric intrusion of 0₃ during winter and pre-monsoon seasons. Observed enhanced O₃ mixing ratio in the upper troposphere is explained by, variation of Potential Vorticity (PV), tropopause pressure, relative humidity and CO-0₃ correlation.

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A11	`02`	`1`		`@1 CHAKRABORTY (T.)`
A11	`03`	`1`		`@1 BEIG (G.)`
A14	`01`			`@1 Indian Institute of Tropical Meteorology @2 Pune @3 IND @Z 1 aut. @Z 2 aut. @Z 3 aut.`
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A64	`01`	`1`		`@0 Annales geophysicae : (1988)`
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C01	`01`		`ENG`	@0 The Model for Ozone and Related chemical Tracers-2 (MOZART-2) is used to examine the evolution of pollutant O₃ in the upper troposphere over the Indian region. Vertical profiles of ozone mixing ratio retrieved from Microwave Limb Sounder (MLS) aboard Earth Observing System (EOS) AURA satellite for the period 2005-2009 and Tropospheric Emission Spectrometer (TES) aboard (EOS) AURA for the period 2006-2007 has been analyzed. The satellite observations reveal the evidence of downward propagation of ozone (100-200 ppb) due to stratospheric intrusion during the winter and pre-monsoon seasons. The regular feature of enhancement of ozone in the upper troposphere over India is presented. Results obtained by the MOZART-2 simulations (for years 2000-2005) confirm the observations and indicate stratospheric intrusion of 0₃ during winter and pre-monsoon seasons. Observed enhanced O₃ mixing ratio in the upper troposphere is explained by, variation of Potential Vorticity (PV), tropopause pressure, relative humidity and CO-0₃ correlation.
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C03	`04`	`2`	`FRE`	`@0 Inde @2 NG @5 29`
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C03	`04`	`2`	`SPA`	`@0 India @2 NG @5 29`
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C03	`06`	`2`	`FRE`	`@0 Traceur @5 31`
C03	`06`	`2`	`ENG`	`@0 tracers @5 31`
C03	`06`	`2`	`SPA`	`@0 Trazador @5 31`
C03	`07`	`X`	`FRE`	`@0 Répartition altitudinale @5 32`
C03	`07`	`X`	`ENG`	`@0 Altitudinal distribution @5 32`
C03	`07`	`X`	`SPA`	`@0 Distribución de altitud @5 32`
C03	`08`	`X`	`FRE`	`@0 Rapport mélange @5 33`
C03	`08`	`X`	`ENG`	`@0 Mixing ratio @5 33`
C03	`08`	`X`	`SPA`	`@0 Relación mezcla @5 33`
C03	`09`	`X`	`FRE`	`@0 Observation par satellite @5 34`
C03	`09`	`X`	`ENG`	`@0 Satellite observation @5 34`
C03	`09`	`X`	`SPA`	`@0 Observación por satélite @5 34`
C03	`10`	`X`	`FRE`	`@0 Mousson hiver @5 35`
C03	`10`	`X`	`ENG`	`@0 Winter monsoon @5 35`
C03	`10`	`X`	`SPA`	`@0 Monzón invierno @5 35`
C03	`11`	`X`	`FRE`	`@0 Tourbillon potentiel @5 36`
C03	`11`	`X`	`ENG`	`@0 Potential vorticity @5 36`
C03	`11`	`X`	`SPA`	`@0 Vorticidad potencial @5 36`
C03	`12`	`X`	`FRE`	`@0 Tropopause @5 37`
C03	`12`	`X`	`ENG`	`@0 Tropopause @5 37`
C03	`12`	`X`	`SPA`	`@0 Tropopausa @5 37`
C03	`13`	`X`	`FRE`	`@0 Humidité relative @5 38`
C03	`13`	`X`	`ENG`	`@0 Relative humidity @5 38`
C03	`13`	`X`	`SPA`	`@0 Humedad relativa @5 38`
C03	`14`	`2`	`FRE`	`@0 Corrélation @5 39`
C03	`14`	`2`	`ENG`	`@0 correlation @5 39`
C03	`14`	`2`	`SPA`	`@0 Correlación @5 39`
C03	`15`	`3`	`FRE`	`@0 Structure atmosphérique @5 40`
C03	`15`	`3`	`ENG`	`@0 Atmospheric structure @5 40`
C03	`16`	`3`	`FRE`	`@0 Composition atmosphérique @5 41`
C03	`16`	`3`	`ENG`	`@0 Atmospheric composition @5 41`
C03	`17`	`2`	`FRE`	`@0 Télédétection spatiale @5 42`
C03	`17`	`2`	`ENG`	`@0 Space remote sensing @5 42`
C03	`17`	`2`	`SPA`	`@0 Teledetección espacial @5 42`
C03	`18`	`2`	`FRE`	`@0 Sondeur du limbe en hyperfréquence @4 CD @5 96`
C03	`18`	`2`	`ENG`	`@0 Microwave limb sounder @4 CD @5 96`
C07	`01`	`2`	`FRE`	`@0 Asie @2 564`
C07	`01`	`2`	`ENG`	`@0 Asia @2 564`
C07	`01`	`2`	`SPA`	`@0 Asia @2 564`
N21				`@1 024`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Le document en format XML

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<term>Mixing ratio</term>
<term>Potential vorticity</term>
<term>Relative humidity</term>
<term>Satellite observation</term>
<term>Space remote sensing</term>
<term>Tropopause</term>
<term>Winter monsoon</term>
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<term>Répartition altitudinale</term>
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<front><div type="abstract" xml:lang="en">The Model for Ozone and Related chemical Tracers-2 (MOZART-2) is used to examine the evolution of pollutant O<sub>3</sub>
 in the upper troposphere over the Indian region. Vertical profiles of ozone mixing ratio retrieved from Microwave Limb Sounder (MLS) aboard Earth Observing System (EOS) AURA satellite for the period 2005-2009 and Tropospheric Emission Spectrometer (TES) aboard (EOS) AURA for the period 2006-2007 has been analyzed. The satellite observations reveal the evidence of downward propagation of ozone (100-200 ppb) due to stratospheric intrusion during the winter and pre-monsoon seasons. The regular feature of enhancement of ozone in the upper troposphere over India is presented. Results obtained by the MOZART-2 simulations (for years 2000-2005) confirm the observations and indicate stratospheric intrusion of 0<sub>3</sub>
 during winter and pre-monsoon seasons. Observed enhanced O<sub>3</sub>
 mixing ratio in the upper troposphere is explained by, variation of Potential Vorticity (PV), tropopause pressure, relative humidity and CO-0<sub>3</sub>
 correlation.</div>
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<fA11 i1="02" i2="1"><s1>CHAKRABORTY (T.)</s1>
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<fA14 i1="01"><s1>Indian Institute of Tropical Meteorology</s1>
<s2>Pune</s2>
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<fC01 i1="01" l="ENG"><s0>The Model for Ozone and Related chemical Tracers-2 (MOZART-2) is used to examine the evolution of pollutant O<sub>3</sub>
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 during winter and pre-monsoon seasons. Observed enhanced O<sub>3</sub>
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<fC03 i1="03" i2="2" l="ENG"><s0>troposphere</s0>
<s5>28</s5>
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<fC03 i1="04" i2="2" l="FRE"><s0>Inde</s0>
<s2>NG</s2>
<s5>29</s5>
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<fC03 i1="04" i2="2" l="ENG"><s0>India</s0>
<s2>NG</s2>
<s5>29</s5>
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<fC03 i1="04" i2="2" l="SPA"><s0>India</s0>
<s2>NG</s2>
<s5>29</s5>
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<fC03 i1="05" i2="2" l="FRE"><s0>Modèle</s0>
<s5>30</s5>
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<fC03 i1="05" i2="2" l="ENG"><s0>models</s0>
<s5>30</s5>
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<fC03 i1="05" i2="2" l="SPA"><s0>Modelo</s0>
<s5>30</s5>
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<fC03 i1="06" i2="2" l="FRE"><s0>Traceur</s0>
<s5>31</s5>
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<fC03 i1="06" i2="2" l="ENG"><s0>tracers</s0>
<s5>31</s5>
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<fC03 i1="06" i2="2" l="SPA"><s0>Trazador</s0>
<s5>31</s5>
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<s5>32</s5>
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<fC03 i1="07" i2="X" l="ENG"><s0>Altitudinal distribution</s0>
<s5>32</s5>
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<s5>32</s5>
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<s5>33</s5>
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<fC03 i1="08" i2="X" l="ENG"><s0>Mixing ratio</s0>
<s5>33</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Relación mezcla</s0>
<s5>33</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Observation par satellite</s0>
<s5>34</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Satellite observation</s0>
<s5>34</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Observación por satélite</s0>
<s5>34</s5>
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<fC03 i1="10" i2="X" l="FRE"><s0>Mousson hiver</s0>
<s5>35</s5>
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<fC03 i1="10" i2="X" l="ENG"><s0>Winter monsoon</s0>
<s5>35</s5>
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<fC03 i1="10" i2="X" l="SPA"><s0>Monzón invierno</s0>
<s5>35</s5>
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<fC03 i1="11" i2="X" l="FRE"><s0>Tourbillon potentiel</s0>
<s5>36</s5>
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<fC03 i1="11" i2="X" l="ENG"><s0>Potential vorticity</s0>
<s5>36</s5>
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<fC03 i1="11" i2="X" l="SPA"><s0>Vorticidad potencial</s0>
<s5>36</s5>
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<fC03 i1="12" i2="X" l="FRE"><s0>Tropopause</s0>
<s5>37</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Tropopause</s0>
<s5>37</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Tropopausa</s0>
<s5>37</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Humidité relative</s0>
<s5>38</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Relative humidity</s0>
<s5>38</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Humedad relativa</s0>
<s5>38</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Corrélation</s0>
<s5>39</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>correlation</s0>
<s5>39</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Correlación</s0>
<s5>39</s5>
</fC03>
<fC03 i1="15" i2="3" l="FRE"><s0>Structure atmosphérique</s0>
<s5>40</s5>
</fC03>
<fC03 i1="15" i2="3" l="ENG"><s0>Atmospheric structure</s0>
<s5>40</s5>
</fC03>
<fC03 i1="16" i2="3" l="FRE"><s0>Composition atmosphérique</s0>
<s5>41</s5>
</fC03>
<fC03 i1="16" i2="3" l="ENG"><s0>Atmospheric composition</s0>
<s5>41</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Télédétection spatiale</s0>
<s5>42</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>Space remote sensing</s0>
<s5>42</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Teledetección espacial</s0>
<s5>42</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Sondeur du limbe en hyperfréquence</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>Microwave limb sounder</s0>
<s4>CD</s4>
<s5>96</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>024</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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   |texte=   Seasonal stratospheric intrusion of ozone in the upper troposphere over India
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Seasonal stratospheric intrusion of ozone in the upper troposphere over India

Seasonal stratospheric intrusion of ozone in the upper troposphere over India

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