On the Dynamics of Indian Ocean Teleconnections into the Southern Hemisphere during Austral Winter

dc.contributor.author	Z. E. Gillett
dc.contributor.author	H. H. Hendon
dc.contributor.author	J. M. Arblaster
dc.contributor.author	H. Lin
dc.contributor.author	D. Fuchs
dc.date.accessioned	2023-04-12T18:32:48Z
dc.date.available	2023-04-12T18:32:48Z
dc.date.copyright	2022/09/01
dc.date.issued	2022
dc.identifier.other	JAS-D-21-0206.1.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl1/handle/yetl/4289855
dc.description.abstract	Stationary Rossby waves, forced by the Indian Ocean dipole (IOD), have an important role in Southern Hemisphere (SH) weather and climate, including promoting Australian drought and driving Antarctic sea ice variations. However, the dynamics of these teleconnections are not fully understood. During winter, the subtropical jet (STJ) should prohibit continuous propagation of a stationary Rossby wave into the SH extratropics due to the negative meridional gradient of absolute vorticity (
dc.publisher	American Meteorological Society
dc.title	On the Dynamics of Indian Ocean Teleconnections into the Southern Hemisphere during Austral Winter
dc.type	Journal Paper
dc.journal.volume	79
dc.journal.issue	9
dc.journal.title	Journal of the Atmospheric Sciences
dc.identifier.doi	10.1175/JAS-D-21-0206.1
dc.journal.fristpage	2453
dc.journal.lastpage	2469
dc.page	2453–2469
dc.tree	Journal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 009
dc.contenttype	Fulltext