untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T18:24:26Z</responseDate>
<request identifier=oai:HAL:hal-00337060v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-00337060v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:sde</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-STRASBG1</setSpec>
<setSpec>collection:SDE</setSpec>
<setSpec>collection:MNHN</setSpec>
<setSpec>collection:METEO</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:UNIV-STRASBG</setSpec>
<setSpec>collection:UPMC</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:LOCEAN</setSpec>
<setSpec>collection:UVSQ</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:PARVATI</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:UPMC_POLE_3</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
<setSpec>collection:AERONOMIE</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>West African Monsoon observed with ground-based GPS receivers during African Monsoon Multidisciplinary Analysis (AMMA)</title>
<creator>Bock, Olivier</creator>
<creator>Bouin, Marie-Noëlle</creator>
<creator>Doerflinger, E.</creator>
<creator>Collard, P.</creator>
<creator>Masson, F.</creator>
<creator>Meynadier, Rémi</creator>
<creator>Nahmani, Samuel</creator>
<creator>Koité, M.</creator>
<creator>Gaptia Lawan Balawan, K.</creator>
<creator>Didé, F.</creator>
<creator>Ouedraogo, D.</creator>
<creator>Pokperlaar, S.</creator>
<creator>Ngamini, Jean-Blaise</creator>
<creator>Lafore, Jean-Philippe</creator>
<creator>Janicot, Serge</creator>
<creator>Guichard, FranÇoise</creator>
<creator>Nuret, Mathieu</creator>
<contributor>Service d'aéronomie (SA) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire de Recherche en Géodésie, IGN (LAREG) ; Institut géographique national [IGN ]</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Institut de physique du globe de Strasbourg (IPGS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Groupe d'étude de l'atmosphère météorologique (CNRM-GAME) ; Institut national des sciences de l'Univers (INSU - CNRS) - Météo France - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) ; Muséum National d'Histoire Naturelle (MNHN) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>European Community’s Sixth Framework Research Programme</contributor>
<description>International audience</description>
<source>ISSN: 2169-897X</source>
<source>EISSN: 2169-8996</source>
<source>Journal of Geophysical Research: Atmospheres</source>
<publisher>American Geophysical Union</publisher>
<identifier>hal-00337060</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00337060</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00337060/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00337060/file/Bock_et_al-2008-Journalsur Geophysical_Research__Solid_Earth_%281978-2012%29.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00337060</source>
<source>Journal of Geophysical Research: Atmospheres, American Geophysical Union, 2008, 113 (D21), pp.D21105. 〈10.1029/2008JD010327〉</source>
<identifier>DOI : 10.1029/2008JD010327</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2008JD010327</relation>
<language>en</language>
<subject lang=en>GPS</subject>
<subject lang=en>AMMA</subject>
<subject lang=en>West African Monsoon</subject>
<subject>[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The impact of stratospheric ozone on the tropospheric general circulation of theSouthern Hemisphere (SH) is examined with a set of chemistry‐climate models participatingin the Stratospheric Processes and their Role in Climate (SPARC)/Chemistry‐ClimateModel Validation project phase 2 (CCMVal‐2). Model integrations of both the past andfuture climates reveal the crucial role of stratospheric ozone in driving SH circulationchange: stronger ozone depletion in late spring generally leads to greater polewarddisplacement and intensification of the tropospheric midlatitude jet, and greater expansion ofthe SH Hadley cell in the summer. These circulation changes are systematic as polewarddisplacement of the jet is typically accompanied by intensification of the jet and expansion ofthe Hadley cell. Overall results are compared with coupled models participating in theIntergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4), andpossible mechanisms are discussed. While the tropospheric circulation response appearsquasi‐linearly related to stratospheric ozone changes, the quantitative response to a givenforcing varies considerably from one model to another. This scatter partly results fromdifferences in model climatology. It is shown that poleward intensification of the westerly jetis generally stronger in models whose climatological jet is biased toward lower latitudes.This result is discussed in the context of quasi‐geostrophic zonal mean dynamics.</description>
<date>2008</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
