Convectively Generated Negative Potential Vorticity Enhancing the Jet Stream through an Inverse Energy Cascade during the Extratropical Transition of Hurricane Irma

dc.contributor.author	Kevin C. Prince
dc.contributor.author	Clark Evans
dc.date.accessioned	2023-04-12T18:36:12Z
dc.date.available	2023-04-12T18:36:12Z
dc.date.copyright	2022/10/27
dc.date.issued	2022
dc.identifier.other	JAS-D-22-0094.1.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl1/handle/yetl/4289951
dc.description.abstract	A tropical cyclone (TC) that recurves into the midlatitudes can lead to significant downstream flow amplification by way of a favorable interaction with the midlatitude waveguide. Current conceptualizations emphasize the role of the meso-
dc.publisher	American Meteorological Society
dc.title	Convectively Generated Negative Potential Vorticity Enhancing the Jet Stream through an Inverse Energy Cascade during the Extratropical Transition of Hurricane Irma
dc.type	Journal Paper
dc.journal.volume	79
dc.journal.issue	11
dc.journal.title	Journal of the Atmospheric Sciences
dc.identifier.doi	10.1175/JAS-D-22-0094.1
dc.journal.fristpage	2901
dc.journal.lastpage	2918
dc.page	2901–2918
dc.tree	Journal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 011
dc.contenttype	Fulltext