000825118 001__ 825118
000825118 005__ 20240712100840.0
000825118 0247_ $$2doi$$a10.5194/acp-2016-582
000825118 0247_ $$2ISSN$$a1680-7367
000825118 0247_ $$2ISSN$$a1680-7375
000825118 0247_ $$2Handle$$a2128/13631
000825118 0247_ $$2altmetric$$aaltmetric:9870764
000825118 037__ $$aFZJ-2016-07595
000825118 082__ $$a550
000825118 1001_ $$0P:(DE-HGF)0$$aRoy, Chaitri$$b0
000825118 245__ $$aInfluence of enhanced Asian NO$_{x}$ emissions on ozone in the Upper Troposphere and Lower Stratosphere (UTLS) in chemistry climate model simulations
000825118 260__ $$aKatlenburg-Lindau$$bEGU$$c2016
000825118 3367_ $$2DRIVER$$aarticle
000825118 3367_ $$2DataCite$$aOutput Types/Journal article
000825118 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1485421338_32147
000825118 3367_ $$2BibTeX$$aARTICLE
000825118 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000825118 3367_ $$00$$2EndNote$$aJournal Article
000825118 520__ $$aAsian summer monsoon convection plays an important role in efficient vertical transport from the surface to the anticyclone. In this paper we investigate the potential impact of convectively transported anthropogenic nitrogen oxides (NOx) on the distribution of ozone in the Upper Troposphere and Lower Stratosphere (UTLS) from simulations with the fully-coupled aerosol chemistry climate model, ECHAM5-HAMMOZ. We performed anthropogenic NOx emission sensitivity experiments over India and China. In these simulations, anthropogenic NOx emissions for the period 2000–2010 have been increased by 38 % over India and by 73 % over China in accordance with satellite observed trends over India of 3.8 % per year and China of 7.3 % per year. These NOx emission sensitivity simulations show that strong convection over the Bay of Bengal and the Southern slopes of the Himalayas transports Indian emissions into the UTLS. Convective transport from the South China Sea injects Chinese emissions into the lower stratosphere. Indian and Chinese emissions are partially transported over the Arabian Sea and west Asia by the tropical easterly jet. Enhanced NOx emissions over India and China increase the ozone radiative forcing over India by 0.112 W/m2 and 0.121 W/m2 respectively. These elevated emissions produces significant warming over the Tibetan Plateau and increase precipitation over India due to a strengthening of the monsoon Hadley circulation.However doubling of NOx emissions over India (73 %); equal to China, produced high ozone in the lower troposphere. It induced a reverse monsoon Hadley circulation and negative precipitation anomalies over India. The associated subsidence suppressed vertical transport of NOx and ozone into the anticyclone.
000825118 536__ $$0G:(DE-HGF)POF3-244$$a244 - Composition and dynamics of the upper troposphere and middle atmosphere (POF3-244)$$cPOF3-244$$fPOF III$$x0
000825118 588__ $$aDataset connected to CrossRef
000825118 7001_ $$0P:(DE-HGF)0$$aFadnavis, Suvarna$$b1$$eCorresponding author
000825118 7001_ $$0P:(DE-Juel1)129138$$aMüller, Rolf$$b2$$ufzj
000825118 7001_ $$0P:(DE-HGF)0$$aChaudhary, Ayantika Dey$$b3
000825118 7001_ $$0P:(DE-Juel1)129141$$aPloeger, Felix$$b4$$ufzj
000825118 773__ $$0PERI:(DE-600)2069857-4$$a10.5194/acp-2016-582$$gp. 1 - 29$$p $$tAtmospheric chemistry and physics / Discussions$$v $$x1680-7375$$y2016
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.pdf$$yOpenAccess
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.gif?subformat=icon$$xicon$$yOpenAccess
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.jpg?subformat=icon-1440$$xicon-1440$$yOpenAccess
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.jpg?subformat=icon-180$$xicon-180$$yOpenAccess
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.jpg?subformat=icon-640$$xicon-640$$yOpenAccess
000825118 8564_ $$uhttps://juser.fz-juelich.de/record/825118/files/acp-2016-582.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000825118 909CO $$ooai:juser.fz-juelich.de:825118$$pdnbdelivery$$pVDB$$pdriver$$popen_access$$popenaire
000825118 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129138$$aForschungszentrum Jülich$$b2$$kFZJ
000825118 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129141$$aForschungszentrum Jülich$$b4$$kFZJ
000825118 9131_ $$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$$x0
000825118 9141_ $$y2016
000825118 915__ $$0LIC:(DE-HGF)CCBY3$$2HGFVOC$$aCreative Commons Attribution CC BY 3.0
000825118 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal
000825118 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ
000825118 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000825118 915__ $$0StatID:(DE-HGF)0310$$2StatID$$aDBCoverage$$bNCBI Molecular Biology Database
000825118 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline
000825118 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$kIEK-7$$lStratosphäre$$x0
000825118 9801_ $$aFullTexts
000825118 980__ $$ajournal
000825118 980__ $$aVDB
000825118 980__ $$aUNRESTRICTED
000825118 980__ $$aI:(DE-Juel1)IEK-7-20101013
000825118 981__ $$aI:(DE-Juel1)ICE-4-20101013