Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation
Identifieur interne : 000207 ( PascalFrancis/Corpus ); précédent : 000206; suivant : 000208Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation
Auteurs : JIANZHONG MA ; HONGLI LIU ; Didier HauglustaineSource :
- Journal of geophysical research [ 0148-0227 ] ; 2002.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
[i] A three-dimensional regional chemical transport model, extended from the Regional Acid Deposition Model (RADM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors over China, is presented. The model domain covers the China region with a horizontal resolution of 100 km. In the vertical, the model extends up to the pressure level of 10 mbar for meteorological simulation, and to the local thermal tropopause for chemical integration. The meteorological fields for the model run are provided with the Fifth-Generation National Center for Atmospheric Research (NCAR)/ Penn State Mesoscale Model (MM5). In addition to updated surface emissions, aircraft emissions and lightning NOx sources are taken into account. The initial fields and lateral boundary conditions for most chemical tracers are provided with a global chemical transport model for ozone and related chemical tracers (MOZART). The model simulation is performed for the period July 1-15, 1995, which appears to be representative of meteorological conditions in summertime over China. The model results are compared with surface measurements of ozone and its precursors in China, ozone soundings in Japan, and MOZART results for the China region. The daily variation as well as geographical and vertical distribution of O3 concentration is generally well simulated by the model. It is indicated that surface ozone is controlled by photochemistry in eastern China and by transport processes in western China. Large-scale transport of O3 and its precursors from the highest-source-emission regions to remote areas and the free troposphere is simulated.
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Pour connaître la documentation sur le format Inist Standard.
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Format Inist (serveur)
| NO : | PASCAL 03-0302870 INIST |
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| ET : | Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation |
| AU : | JIANZHONG MA; HONGLI LIU; HAUGLUSTAINE (Didier) |
| AF : | Chinese Academy of Meteorological Sciences/Beijing/Chine (1 aut., 2 aut.); Service d'Aéronomie du Centre National de la Recherche Scientifique/Paris/France (3 aut.) |
| DT : | Publication en série; Niveau analytique |
| SO : | Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2002; Vol. 107; No. D22; ACH27.1-ACH27.13; Bibl. 53 ref. |
| LA : | Anglais |
| EA : | [i] A three-dimensional regional chemical transport model, extended from the Regional Acid Deposition Model (RADM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors over China, is presented. The model domain covers the China region with a horizontal resolution of 100 km. In the vertical, the model extends up to the pressure level of 10 mbar for meteorological simulation, and to the local thermal tropopause for chemical integration. The meteorological fields for the model run are provided with the Fifth-Generation National Center for Atmospheric Research (NCAR)/ Penn State Mesoscale Model (MM5). In addition to updated surface emissions, aircraft emissions and lightning NOx sources are taken into account. The initial fields and lateral boundary conditions for most chemical tracers are provided with a global chemical transport model for ozone and related chemical tracers (MOZART). The model simulation is performed for the period July 1-15, 1995, which appears to be representative of meteorological conditions in summertime over China. The model results are compared with surface measurements of ozone and its precursors in China, ozone soundings in Japan, and MOZART results for the China region. The daily variation as well as geographical and vertical distribution of O3 concentration is generally well simulated by the model. It is indicated that surface ozone is controlled by photochemistry in eastern China and by transport processes in western China. Large-scale transport of O3 and its precursors from the highest-source-emission regions to remote areas and the free troposphere is simulated. |
| CC : | 001E02D04; 001D16C02 |
| FD : | Troposphère; Ozone; Simulation numérique; Précurseur; Tropopause; Condition météorologique; Variation journalière; Répartition géographique; Distribution concentration; Photochimie; Phénomène transport; Eté; Modèle 3 dimensions; Azote oxyde; Chine; Japon |
| FG : | Asie |
| ED : | Troposphere; Ozone; Numerical simulation; Precursor; Tropopause; Atmospheric condition; Daily variation; Geographic distribution; Concentration distribution; Photochemistry; Transport process; Summer; Three dimensional model; Nitrogen oxide; China; Japan |
| EG : | Asia |
| SD : | Troposfera; Ozono; Simulación numérica; Precursor; Tropopausa; Condición meteorológica; Variación diaria; Distribución geográfica; Distribución concentración; Fotoquímica; Fenómeno transporte; Verano; Modelo 3 dimensiones; Nitrógeno óxido; China; Japón |
| LO : | INIST-3144.354000104212210560 |
| ID : | 03-0302870 |
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<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation</title><author><name sortKey="Jianzhong Ma" sort="Jianzhong Ma" uniqKey="Jianzhong Ma" last="Jianzhong Ma">JIANZHONG MA</name><affiliation><inist:fA14 i1="01"><s1>Chinese Academy of Meteorological Sciences</s1><s2>Beijing</s2><s3>CHN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Hongli Liu" sort="Hongli Liu" uniqKey="Hongli Liu" last="Hongli Liu">HONGLI LIU</name><affiliation><inist:fA14 i1="01"><s1>Chinese Academy of Meteorological Sciences</s1><s2>Beijing</s2><s3>CHN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Hauglustaine, Didier" sort="Hauglustaine, Didier" uniqKey="Hauglustaine D" first="Didier" last="Hauglustaine">Didier Hauglustaine</name><affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1><s2>Paris</s2><s3>FRA</s3><sZ>3 aut.</sZ></inist:fA14></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">03-0302870</idno><date when="2002">2002</date><idno type="stanalyst">PASCAL 03-0302870 INIST</idno><idno type="RBID">Pascal:03-0302870</idno><idno type="wicri:Area/PascalFrancis/Corpus">000207</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation</title><author><name sortKey="Jianzhong Ma" sort="Jianzhong Ma" uniqKey="Jianzhong Ma" last="Jianzhong Ma">JIANZHONG MA</name><affiliation><inist:fA14 i1="01"><s1>Chinese Academy of Meteorological Sciences</s1><s2>Beijing</s2><s3>CHN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Hongli Liu" sort="Hongli Liu" uniqKey="Hongli Liu" last="Hongli Liu">HONGLI LIU</name><affiliation><inist:fA14 i1="01"><s1>Chinese Academy of Meteorological Sciences</s1><s2>Beijing</s2><s3>CHN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Hauglustaine, Didier" sort="Hauglustaine, Didier" uniqKey="Hauglustaine D" first="Didier" last="Hauglustaine">Didier Hauglustaine</name><affiliation><inist:fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1><s2>Paris</s2><s3>FRA</s3><sZ>3 aut.</sZ></inist:fA14></affiliation></author></analytic><series><title level="j" type="main">Journal of geophysical research</title><title level="j" type="abbreviated">J. geophys. res.</title><idno type="ISSN">0148-0227</idno><imprint><date when="2002">2002</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of geophysical research</title><title level="j" type="abbreviated">J. geophys. res.</title><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Atmospheric condition</term><term>China</term><term>Concentration distribution</term><term>Daily variation</term><term>Geographic distribution</term><term>Japan</term><term>Nitrogen oxide</term><term>Numerical simulation</term><term>Ozone</term><term>Photochemistry</term><term>Precursor</term><term>Summer</term><term>Three dimensional model</term><term>Transport process</term><term>Tropopause</term><term>Troposphere</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Troposphère</term><term>Ozone</term><term>Simulation numérique</term><term>Précurseur</term><term>Tropopause</term><term>Condition météorologique</term><term>Variation journalière</term><term>Répartition géographique</term><term>Distribution concentration</term><term>Photochimie</term><term>Phénomène transport</term><term>Eté</term><term>Modèle 3 dimensions</term><term>Azote oxyde</term><term>Chine</term><term>Japon</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">[i] A three-dimensional regional chemical transport model, extended from the Regional Acid Deposition Model (RADM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors over China, is presented. The model domain covers the China region with a horizontal resolution of 100 km. In the vertical, the model extends up to the pressure level of 10 mbar for meteorological simulation, and to the local thermal tropopause for chemical integration. The meteorological fields for the model run are provided with the Fifth-Generation National Center for Atmospheric Research (NCAR)/ Penn State Mesoscale Model (MM5). In addition to updated surface emissions, aircraft emissions and lightning NO<sub>x</sub> sources are taken into account. The initial fields and lateral boundary conditions for most chemical tracers are provided with a global chemical transport model for ozone and related chemical tracers (MOZART). The model simulation is performed for the period July 1-15, 1995, which appears to be representative of meteorological conditions in summertime over China. The model results are compared with surface measurements of ozone and its precursors in China, ozone soundings in Japan, and MOZART results for the China region. The daily variation as well as geographical and vertical distribution of O<sub>3</sub> concentration is generally well simulated by the model. It is indicated that surface ozone is controlled by photochemistry in eastern China and by transport processes in western China. Large-scale transport of O<sub>3</sub> and its precursors from the highest-source-emission regions to remote areas and the free troposphere is simulated.</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>107</s2></fA05><fA06><s2>D22</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation</s1></fA08><fA11 i1="01" i2="1"><s1>JIANZHONG MA</s1></fA11><fA11 i1="02" i2="1"><s1>HONGLI LIU</s1></fA11><fA11 i1="03" i2="1"><s1>HAUGLUSTAINE (Didier)</s1></fA11><fA14 i1="01"><s1>Chinese Academy of Meteorological Sciences</s1><s2>Beijing</s2><s3>CHN</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></fA14><fA14 i1="02"><s1>Service d'Aéronomie du Centre National de la Recherche Scientifique</s1><s2>Paris</s2><s3>FRA</s3><sZ>3 aut.</sZ></fA14><fA20><s2>ACH27.1-ACH27.13</s2></fA20><fA21><s1>2002</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>3144</s2><s5>354000104212210560</s5></fA43><fA44><s0>0000</s0><s1>© 2003 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>53 ref.</s0></fA45><fA47 i1="01" i2="1"><s0>03-0302870</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>[i] A three-dimensional regional chemical transport model, extended from the Regional Acid Deposition Model (RADM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors over China, is presented. The model domain covers the China region with a horizontal resolution of 100 km. In the vertical, the model extends up to the pressure level of 10 mbar for meteorological simulation, and to the local thermal tropopause for chemical integration. The meteorological fields for the model run are provided with the Fifth-Generation National Center for Atmospheric Research (NCAR)/ Penn State Mesoscale Model (MM5). In addition to updated surface emissions, aircraft emissions and lightning NO<sub>x</sub> sources are taken into account. The initial fields and lateral boundary conditions for most chemical tracers are provided with a global chemical transport model for ozone and related chemical tracers (MOZART). The model simulation is performed for the period July 1-15, 1995, which appears to be representative of meteorological conditions in summertime over China. The model results are compared with surface measurements of ozone and its precursors in China, ozone soundings in Japan, and MOZART results for the China region. The daily variation as well as geographical and vertical distribution of O<sub>3</sub> concentration is generally well simulated by the model. It is indicated that surface ozone is controlled by photochemistry in eastern China and by transport processes in western China. Large-scale transport of O<sub>3</sub> and its precursors from the highest-source-emission regions to remote areas and the free troposphere is simulated.</s0></fC01><fC02 i1="01" i2="X"><s0>001E02D04</s0></fC02><fC02 i1="02" i2="X"><s0>001D16C02</s0></fC02><fC03 i1="01" i2="X" l="FRE"><s0>Troposphère</s0><s5>26</s5></fC03><fC03 i1="01" i2="X" l="ENG"><s0>Troposphere</s0><s5>26</s5></fC03><fC03 i1="01" i2="X" l="SPA"><s0>Troposfera</s0><s5>26</s5></fC03><fC03 i1="02" i2="X" l="FRE"><s0>Ozone</s0><s2>NK</s2><s2>FX</s2><s5>27</s5></fC03><fC03 i1="02" i2="X" l="ENG"><s0>Ozone</s0><s2>NK</s2><s2>FX</s2><s5>27</s5></fC03><fC03 i1="02" i2="X" l="SPA"><s0>Ozono</s0><s2>NK</s2><s2>FX</s2><s5>27</s5></fC03><fC03 i1="03" i2="X" l="FRE"><s0>Simulation numérique</s0><s5>28</s5></fC03><fC03 i1="03" i2="X" l="ENG"><s0>Numerical simulation</s0><s5>28</s5></fC03><fC03 i1="03" i2="X" l="SPA"><s0>Simulación numérica</s0><s5>28</s5></fC03><fC03 i1="04" i2="X" l="FRE"><s0>Précurseur</s0><s5>29</s5></fC03><fC03 i1="04" i2="X" l="ENG"><s0>Precursor</s0><s5>29</s5></fC03><fC03 i1="04" i2="X" l="SPA"><s0>Precursor</s0><s5>29</s5></fC03><fC03 i1="05" i2="X" l="FRE"><s0>Tropopause</s0><s5>30</s5></fC03><fC03 i1="05" i2="X" l="ENG"><s0>Tropopause</s0><s5>30</s5></fC03><fC03 i1="05" i2="X" l="SPA"><s0>Tropopausa</s0><s5>30</s5></fC03><fC03 i1="06" i2="X" l="FRE"><s0>Condition météorologique</s0><s5>36</s5></fC03><fC03 i1="06" i2="X" l="ENG"><s0>Atmospheric condition</s0><s5>36</s5></fC03><fC03 i1="06" i2="X" l="SPA"><s0>Condición meteorológica</s0><s5>36</s5></fC03><fC03 i1="07" i2="X" l="FRE"><s0>Variation journalière</s0><s5>37</s5></fC03><fC03 i1="07" i2="X" l="ENG"><s0>Daily variation</s0><s5>37</s5></fC03><fC03 i1="07" i2="X" l="SPA"><s0>Variación diaria</s0><s5>37</s5></fC03><fC03 i1="08" i2="X" l="FRE"><s0>Répartition géographique</s0><s5>38</s5></fC03><fC03 i1="08" i2="X" l="ENG"><s0>Geographic distribution</s0><s5>38</s5></fC03><fC03 i1="08" i2="X" l="SPA"><s0>Distribución geográfica</s0><s5>38</s5></fC03><fC03 i1="09" i2="X" l="FRE"><s0>Distribution concentration</s0><s5>39</s5></fC03><fC03 i1="09" i2="X" l="ENG"><s0>Concentration distribution</s0><s5>39</s5></fC03><fC03 i1="09" i2="X" l="SPA"><s0>Distribución concentración</s0><s5>39</s5></fC03><fC03 i1="10" i2="X" l="FRE"><s0>Photochimie</s0><s5>40</s5></fC03><fC03 i1="10" i2="X" l="ENG"><s0>Photochemistry</s0><s5>40</s5></fC03><fC03 i1="10" i2="X" l="SPA"><s0>Fotoquímica</s0><s5>40</s5></fC03><fC03 i1="11" i2="X" l="FRE"><s0>Phénomène transport</s0><s5>41</s5></fC03><fC03 i1="11" i2="X" l="ENG"><s0>Transport process</s0><s5>41</s5></fC03><fC03 i1="11" i2="X" l="SPA"><s0>Fenómeno transporte</s0><s5>41</s5></fC03><fC03 i1="12" i2="X" l="FRE"><s0>Eté</s0><s5>42</s5></fC03><fC03 i1="12" i2="X" l="ENG"><s0>Summer</s0><s5>42</s5></fC03><fC03 i1="12" i2="X" l="SPA"><s0>Verano</s0><s5>42</s5></fC03><fC03 i1="13" i2="X" l="FRE"><s0>Modèle 3 dimensions</s0><s5>43</s5></fC03><fC03 i1="13" i2="X" l="ENG"><s0>Three dimensional model</s0><s5>43</s5></fC03><fC03 i1="13" i2="X" l="SPA"><s0>Modelo 3 dimensiones</s0><s5>43</s5></fC03><fC03 i1="14" i2="X" l="FRE"><s0>Azote oxyde</s0><s5>44</s5></fC03><fC03 i1="14" i2="X" l="ENG"><s0>Nitrogen oxide</s0><s5>44</s5></fC03><fC03 i1="14" i2="X" l="SPA"><s0>Nitrógeno óxido</s0><s5>44</s5></fC03><fC03 i1="15" i2="X" l="FRE"><s0>Chine</s0><s2>NG</s2><s5>49</s5></fC03><fC03 i1="15" i2="X" l="ENG"><s0>China</s0><s2>NG</s2><s5>49</s5></fC03><fC03 i1="15" i2="X" l="SPA"><s0>China</s0><s2>NG</s2><s5>49</s5></fC03><fC03 i1="16" i2="X" l="FRE"><s0>Japon</s0><s2>NG</s2><s5>50</s5></fC03><fC03 i1="16" i2="X" l="ENG"><s0>Japan</s0><s2>NG</s2><s5>50</s5></fC03><fC03 i1="16" i2="X" l="SPA"><s0>Japón</s0><s2>NG</s2><s5>50</s5></fC03><fC07 i1="01" i2="X" l="FRE"><s0>Asie</s0><s2>NG</s2></fC07><fC07 i1="01" i2="X" l="ENG"><s0>Asia</s0><s2>NG</s2></fC07><fC07 i1="01" i2="X" l="SPA"><s0>Asia</s0><s2>NG</s2></fC07><fN21><s1>202</s1></fN21><fN82><s1>PSI</s1></fN82></pA></standard><server><NO>PASCAL 03-0302870 INIST</NO><ET>Summertime tropospheric ozone over China simulated with a regional chemical transport model. 1. Model description and evaluation</ET><AU>JIANZHONG MA; HONGLI LIU; HAUGLUSTAINE (Didier)</AU><AF>Chinese Academy of Meteorological Sciences/Beijing/Chine (1 aut., 2 aut.); Service d'Aéronomie du Centre National de la Recherche Scientifique/Paris/France (3 aut.)</AF><DT>Publication en série; Niveau analytique</DT><SO>Journal of geophysical research; ISSN 0148-0227; Etats-Unis; Da. 2002; Vol. 107; No. D22; ACH27.1-ACH27.13; Bibl. 53 ref.</SO><LA>Anglais</LA><EA>[i] A three-dimensional regional chemical transport model, extended from the Regional Acid Deposition Model (RADM) and aimed at studying the distribution and budget of tropospheric ozone and its precursors over China, is presented. The model domain covers the China region with a horizontal resolution of 100 km. In the vertical, the model extends up to the pressure level of 10 mbar for meteorological simulation, and to the local thermal tropopause for chemical integration. The meteorological fields for the model run are provided with the Fifth-Generation National Center for Atmospheric Research (NCAR)/ Penn State Mesoscale Model (MM5). In addition to updated surface emissions, aircraft emissions and lightning NO<sub>x</sub> sources are taken into account. The initial fields and lateral boundary conditions for most chemical tracers are provided with a global chemical transport model for ozone and related chemical tracers (MOZART). The model simulation is performed for the period July 1-15, 1995, which appears to be representative of meteorological conditions in summertime over China. The model results are compared with surface measurements of ozone and its precursors in China, ozone soundings in Japan, and MOZART results for the China region. The daily variation as well as geographical and vertical distribution of O<sub>3</sub> concentration is generally well simulated by the model. It is indicated that surface ozone is controlled by photochemistry in eastern China and by transport processes in western China. Large-scale transport of O<sub>3</sub> and its precursors from the highest-source-emission regions to remote areas and the free troposphere is simulated.</EA><CC>001E02D04; 001D16C02</CC><FD>Troposphère; Ozone; Simulation numérique; Précurseur; Tropopause; Condition météorologique; Variation journalière; Répartition géographique; Distribution concentration; Photochimie; Phénomène transport; Eté; Modèle 3 dimensions; Azote oxyde; Chine; Japon</FD><FG>Asie</FG><ED>Troposphere; Ozone; Numerical simulation; Precursor; Tropopause; Atmospheric condition; Daily variation; Geographic distribution; Concentration distribution; Photochemistry; Transport process; Summer; Three dimensional model; Nitrogen oxide; China; Japan</ED><EG>Asia</EG><SD>Troposfera; Ozono; Simulación numérica; Precursor; Tropopausa; Condición meteorológica; Variación diaria; Distribución geográfica; Distribución concentración; Fotoquímica; Fenómeno transporte; Verano; Modelo 3 dimensiones; Nitrógeno óxido; China; Japón</SD><LO>INIST-3144.354000104212210560</LO><ID>03-0302870</ID></server></inist></record>Pour manipuler ce document sous Unix (Dilib)
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