LEADER 02087nam  2200457z- 450 
001 9910346899303321
005 20210212
010   $a1000024940
035   $a(CKB)4920000000101529
035   $a(oapen)https://directory.doabooks.org/handle/20.500.12854/57434
035   $a(oapen)doab57434
035   $a(EXLCZ)994920000000101529
100   $a20202102d2015      |y         0
101 0 $aeng
135   $aurmn|---annan
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 00$aQuantification of the Downstream Impact of Extratropical Transition for Typhoon Jangmi and Other Case Studies
210   $cKIT Scientific Publishing$d2015
215   $a1 online resource (VII, 334 p. p.)
225 1 $aWissenschaftliche Berichte des Instituts für Meteorologie und Klimaforschung des Karlsruher Instituts für Technologie
311 08$a3-86644-776-0 
330   $aThe impact of extratropical transition on the midlatitude flow is quantified based on potential vorticity inversion. The detailed study of Typhoon Jangmi (2008) reveals the diabatically enhanced net transport of low-PV air to the tropopause as the key physical process determining the direct impact of ET. Relocation experiments and further case studies show the crucial role of the relative position of the TC and the midlatitude flow for the downstream impact of ET and the reduced predictability.
606   $aPhysics$2bicssc
610   $aAtmospha?rische Dynamik
610   $aAtmospheric Dynamics
610   $ajet stream
610   $amidlatitudes
610   $amittlere Breiten
610   $apotential vorticity inversion
610   $aPotentielle Vorticity Inversion
610   $aStrahlstrom
610   $aTropical Cyclone
610   $aTropischer Wirbelsturm
615  7$aPhysics
700   $aGrams$b Christian Michael Warnfrid$4auth$01312102
906   $aBOOK
912   $a9910346899303321
996   $aQuantification of the Downstream Impact of Extratropical Transition for Typhoon Jangmi and Other Case Studies$93030686
997   $aUNINA