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000155472 0247_ $$2doi$$a10.5194/acpd-14-18461-2014
000155472 0247_ $$2ISSN$$a1680-7367
000155472 0247_ $$2ISSN$$a1680-7375
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000155472 037__ $$aFZJ-2014-04638
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000155472 1001_ $$0P:(DE-Juel1)129164$$aVogel, B.$$b0$$eCorresponding Author$$ufzj
000155472 245__ $$aFast transport from Southeast Asia boundary layer sources to Northern Europe: rapid uplift in typhoons and eastward eddy shedding of the Asian monsoon anticyclone2
000155472 260__ $$aKatlenburg-Lindau$$bEGU$$c2014
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000155472 520__ $$aDuring the TACTS aircraft campaign enhanced tropospheric trace gases such as CO, CH4, and H2O and reduced stratospheric O3 were measured in situ in the lowermost stratosphere over Northern Europe on 26 September 2012. The measurements indicate that these air masses differ from the stratospheric background. The calculation of 40 day backward trajectories with the trajectory module of the CLaMS model shows that these air masses are affected by the Asian monsoon anticyclone. Some air masses originate from the boundary layer in Southeast Asia/West Pacific and are rapidly lifted (1–2 days) within a typhoon. Afterwards they are injected directly into the anticyclonic circulation of the Asian monsoon. The subsequent long-range transport (8–14 days) of enhanced water vapour and pollutants to the lowermost stratosphere in Northern Europe is driven by eastward transport of tropospheric air from the Asian monsoon anticyclone caused by an eddy shedding event. We find that the combination of rapid uplift by a typhoon and eastward eddy shedding from the Asian monsoon anticyclone is an additional fast transport pathway that, in this study, carries boundary emissions from Southeast Asia/West Pacific within approximately 5 weeks to the lowermost stratosphere in Northern Europe.
000155472 536__ $$0G:(DE-HGF)POF2-234$$a234 - Composition and Dynamics of the Upper Troposphere and Stratosphere (POF2-234)$$cPOF2-234$$fPOF II$$x0
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000155472 7001_ $$0P:(DE-Juel1)129123$$aGünther, G.$$b1$$ufzj
000155472 7001_ $$0P:(DE-Juel1)129138$$aMüller, Rolf$$b2$$ufzj
000155472 7001_ $$0P:(DE-Juel1)129122$$aGrooß, J.-U.$$b3$$ufzj
000155472 7001_ $$0P:(DE-HGF)0$$aHoor, P.$$b4
000155472 7001_ $$0P:(DE-Juel1)162237$$aKrämer, M.$$b5$$ufzj
000155472 7001_ $$0P:(DE-HGF)0$$aMüller, S.$$b6
000155472 7001_ $$0P:(DE-HGF)0$$aZahn, A.$$b7
000155472 7001_ $$0P:(DE-Juel1)129145$$aRiese, M.$$b8$$ufzj
000155472 773__ $$0PERI:(DE-600)2069857-4$$a10.5194/acpd-14-18461-2014$$gVol. 14, no. 12, p. 18461 - 18497$$n12$$p18461 - 18497$$tAtmospheric chemistry and physics / Discussions$$v14$$x1680-7375$$y2014
000155472 8564_ $$uhttp://www.atmos-chem-phys-discuss.net/14/18461/2014/
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000155472 9132_ $$0G:(DE-HGF)POF3-244$$1G:(DE-HGF)POF3-240$$2G:(DE-HGF)POF3-200$$aDE-HGF$$bMarine, Küsten- und Polare Systeme$$lAtmosphäre und Klima$$vComposition and dynamics of the upper troposphere and middle atmosphere$$x0
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000155472 9141_ $$y2014
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