000826977 001__ 826977
000826977 005__ 20240712100909.0
000826977 0247_ $$2doi$$a10.5194/acp-17-1297-2017
000826977 0247_ $$2ISSN$$a1680-7316
000826977 0247_ $$2ISSN$$a1680-7324
000826977 0247_ $$2Handle$$a2128/14321
000826977 0247_ $$2WOS$$aWOS:000394604000004
000826977 0247_ $$2altmetric$$aaltmetric:15864837
000826977 037__ $$aFZJ-2017-01184
000826977 082__ $$a550
000826977 1001_ $$0P:(DE-HGF)0$$aRoy, Chaitri$$b0
000826977 245__ $$aInfluence of enhanced Asian NO<sub><i>x</i></sub> emissions on ozone in the upper troposphere and lower stratosphere in chemistry&ndash;climate model simulations
000826977 260__ $$aKatlenburg-Lindau$$bEGU$$c2017
000826977 3367_ $$2DRIVER$$aarticle
000826977 3367_ $$2DataCite$$aOutput Types/Journal article
000826977 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1493817287_27254
000826977 3367_ $$2BibTeX$$aARTICLE
000826977 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000826977 3367_ $$00$$2EndNote$$aJournal Article
000826977 520__ $$aThe Asian summer monsoon (ASM) anticyclone is the most pronounced circulation pattern in the upper troposphere and lower stratosphere (UTLS) during northern hemispheric summer. ASM convection plays an important role in efficient vertical transport from the surface to the upper-level anticyclone. In this paper we investigate the potential impact of enhanced anthropogenic nitrogen oxide (NOx) emissions on the distribution of ozone in the UTLS using the fully coupled aerosol–chemistry–climate model, ECHAM5-HAMMOZ. Ozone in the UTLS is influenced both by the convective uplift of ozone precursors and by the uplift of enhanced-NOx-induced tropospheric ozone anomalies. We performed anthropogenic NOx emission sensitivity experiments over India and China. In these simulations, covering the years 2000–2010, anthropogenic NOx emissions have been increased by 38 % over India and by 73 % over China with respect to the emission base year 2000. These emission increases are comparable to the observed linear trends of 3.8 % per year over India and 7.3 % per year over China during the period 2000 to 2010. Enhanced NOx emissions over India by 38 % and China by 73 % increase the ozone radiative forcing in the ASM anticyclone (15–40° N, 60–120° E) by 16.3 and 78.5 mW m−2 respectively. These elevated NOx emissions produce significant warming over the Tibetan Plateau and increase precipitation over India due to a strengthening of the monsoon Hadley circulation. However, increase in NOx emissions over India by 73 % (similar to the observed increase over China) results in large ozone production over the Indo-Gangetic Plain and Tibetan Plateau. The higher ozone concentrations, in turn, induce a reversed monsoon Hadley circulation and negative precipitation anomalies over India. The associated subsidence suppresses vertical transport of NOx and ozone into the ASM anticyclone. 
000826977 536__ $$0G:(DE-HGF)POF3-244$$a244 - Composition and dynamics of the upper troposphere and middle atmosphere (POF3-244)$$cPOF3-244$$fPOF III$$x0
000826977 588__ $$aDataset connected to CrossRef
000826977 7001_ $$0P:(DE-HGF)0$$aFadnavis, Suvarna$$b1$$eCorresponding author
000826977 7001_ $$0P:(DE-Juel1)129138$$aMüller, Rolf$$b2
000826977 7001_ $$0P:(DE-HGF)0$$aAyantika, D. C.$$b3
000826977 7001_ $$0P:(DE-Juel1)129141$$aPloeger, Felix$$b4$$ufzj
000826977 7001_ $$0P:(DE-HGF)0$$aRap, Alexandru$$b5
000826977 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-17-1297-2017$$gVol. 17, no. 2, p. 1297 - 1311$$n2$$p1297 - 1311$$tAtmospheric chemistry and physics$$v17$$x1680-7324$$y2017
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.pdf$$yOpenAccess
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.gif?subformat=icon$$xicon$$yOpenAccess
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.jpg?subformat=icon-1440$$xicon-1440$$yOpenAccess
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.jpg?subformat=icon-180$$xicon-180$$yOpenAccess
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.jpg?subformat=icon-640$$xicon-640$$yOpenAccess
000826977 8564_ $$uhttps://juser.fz-juelich.de/record/826977/files/acp-17-1297-2017.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000826977 909CO $$ooai:juser.fz-juelich.de:826977$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000826977 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129138$$aForschungszentrum Jülich$$b2$$kFZJ
000826977 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129141$$aForschungszentrum Jülich$$b4$$kFZJ
000826977 9131_ $$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$$x0
000826977 9141_ $$y2017
000826977 915__ $$0LIC:(DE-HGF)CCBY3$$2HGFVOC$$aCreative Commons Attribution CC BY 3.0
000826977 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000826977 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences
000826977 915__ $$0StatID:(DE-HGF)9905$$2StatID$$aIF >= 5$$bATMOS CHEM PHYS : 2015
000826977 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal
000826977 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ
000826977 915__ $$0StatID:(DE-HGF)0110$$2StatID$$aWoS$$bScience Citation Index
000826977 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000826977 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000826977 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000826977 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bATMOS CHEM PHYS : 2015
000826977 915__ $$0StatID:(DE-HGF)0310$$2StatID$$aDBCoverage$$bNCBI Molecular Biology Database
000826977 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline
000826977 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000826977 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$kIEK-7$$lStratosphäre$$x0
000826977 9801_ $$aFullTexts
000826977 980__ $$ajournal
000826977 980__ $$aVDB
000826977 980__ $$aUNRESTRICTED
000826977 980__ $$aI:(DE-Juel1)IEK-7-20101013
000826977 981__ $$aI:(DE-Juel1)ICE-4-20101013