000256591 001__ 256591
000256591 005__ 20240712100856.0
000256591 0247_ $$2doi$$a10.1155/2015/879578
000256591 0247_ $$2ISSN$$a1687-9309
000256591 0247_ $$2ISSN$$a1687-9317
000256591 0247_ $$2Handle$$a2128/9388
000256591 0247_ $$2WOS$$aWOS:000362020000001
000256591 037__ $$aFZJ-2015-06465
000256591 041__ $$aEnglish
000256591 082__ $$a550
000256591 1001_ $$0P:(DE-HGF)0$$aLiu, Yi$$b0$$eCorresponding author
000256591 245__ $$aDominant Modes of Tropospheric Ozone Variation over East Asia from GOME Observations
000256591 260__ $$aNew York, NY [u.a.]$$bHindawi Publ. Corp.$$c2015
000256591 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1447071172_30060
000256591 3367_ $$2DataCite$$aOutput Types/Journal article
000256591 3367_ $$00$$2EndNote$$aJournal Article
000256591 3367_ $$2BibTeX$$aARTICLE
000256591 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000256591 3367_ $$2DRIVER$$aarticle
000256591 520__ $$aThe variation in tropospheric ozone over East Asia was analyzed using tropospheric column ozone data measured by the Global Ozone Monitoring Experiment (GOME) satellite. An empirical orthogonal function (EOF) analysis was carried out to derive the dominant modes of the variation in the tropospheric ozone volume-mixing ratio (TOVMR). The EOF1 mode, which explained 61.5% of the total variance, showed a same-sign distribution over all of East Asia, with a belt of enhanced ozone concentrations around 40°N. The principal component of EOF1 (PC1) suggested that photochemical ozone production together with Brewer-Dobson circulation and subtropical westerly jet plays important roles in modulating the seasonal variation of the TOVMR; ozone-rich air produced by photochemical processes was transported from the stratosphere to the troposphere by BD circulation and this ozone-rich air was then blocked by the subtropical westerly jet and accumulated north of the jet. The EOF2 mode explained 29.2% of the total variance with an opposite-sign pattern on the north and south side of 35°N. When anticyclonic circulation transported ozone-poor air from the upwelling area over the Bay of Bengal towards the Tibetan Plateau during the onset of the Asian summer monsoon, tropospheric ozone in this region decreased dramatically.
000256591 536__ $$0G:(DE-HGF)POF3-244$$a244 - Composition and dynamics of the upper troposphere and middle atmosphere (POF3-244)$$cPOF3-244$$fPOF III$$x0
000256591 588__ $$aDataset connected to CrossRef
000256591 7001_ $$0P:(DE-HGF)0$$aZhang, Yuli$$b1
000256591 7001_ $$0P:(DE-Juel1)129939$$aWang, Yong$$b2
000256591 7001_ $$0P:(DE-HGF)0$$aLiu, Chuanxi$$b3
000256591 7001_ $$0P:(DE-HGF)0$$aCai, Zhaonan$$b4$$eCorresponding author
000256591 7001_ $$0P:(DE-Juel1)129130$$aKonopka, Paul$$b5
000256591 7001_ $$0P:(DE-Juel1)129138$$aMüller, Rolf$$b6
000256591 773__ $$0PERI:(DE-600)2486777-9$$a10.1155/2015/879578$$gVol. 2015, p. 1 - 10$$p1 - 10$$tAdvances in meteorology$$v2015$$x1687-9317$$y2015
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.pdf$$yOpenAccess
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.gif?subformat=icon$$xicon$$yOpenAccess
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.jpg?subformat=icon-1440$$xicon-1440$$yOpenAccess
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.jpg?subformat=icon-180$$xicon-180$$yOpenAccess
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.jpg?subformat=icon-640$$xicon-640$$yOpenAccess
000256591 8564_ $$uhttps://juser.fz-juelich.de/record/256591/files/879578.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000256591 909CO $$ooai:juser.fz-juelich.de:256591$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000256591 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000256591 915__ $$0LIC:(DE-HGF)CCBY4$$2HGFVOC$$aCreative Commons Attribution CC BY 4.0
000256591 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bADV METEOROL : 2014
000256591 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ
000256591 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000256591 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000256591 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5
000256591 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000256591 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences
000256591 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000256591 9141_ $$y2015
000256591 9101_ $$0I:(DE-HGF)0$$6P:(DE-Juel1)159482$$aExternal Institute$$b0$$kExtern
000256591 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129130$$aForschungszentrum Jülich GmbH$$b5$$kFZJ
000256591 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129138$$aForschungszentrum Jülich GmbH$$b6$$kFZJ
000256591 9131_ $$0G:(DE-HGF)POF3-244$$1G:(DE-HGF)POF3-240$$2G:(DE-HGF)POF3-200$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lAtmosphäre und Klima$$vComposition and dynamics of the upper troposphere and middle atmosphere$$x0
000256591 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$kIEK-7$$lStratosphäre$$x0
000256591 9801_ $$aUNRESTRICTED
000256591 9801_ $$aFullTexts
000256591 980__ $$ajournal
000256591 980__ $$aVDB
000256591 980__ $$aUNRESTRICTED
000256591 980__ $$aI:(DE-Juel1)IEK-7-20101013
000256591 981__ $$aI:(DE-Juel1)ICE-4-20101013