Potential Vorticity and Instability in the Pacific Equatorial Undercurrent West of the Galápagos Archipelago

dc.contributor.author	Julie Jakoboski
dc.contributor.author	Robert E. Todd
dc.contributor.author	W. Brechner Owens
dc.contributor.author	Kristopher B. Karnauskas
dc.contributor.author	Daniel L. Rudnick
dc.date.accessioned	2023-04-12T18:28:44Z
dc.date.available	2023-04-12T18:28:44Z
dc.date.copyright	2022/08/01
dc.date.issued	2022
dc.identifier.other	JPO-D-21-0124.1.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl1/handle/yetl/4289736
dc.description.abstract	The Galápagos Archipelago lies on the equator in the path of the eastward flowing Pacific Equatorial Undercurrent (EUC). When the EUC reaches the archipelago, it upwells and bifurcates into a north and south branch around the archipelago at a latitude determined by topography. Since the Coriolis parameter (
dc.publisher	American Meteorological Society
dc.title	Potential Vorticity and Instability in the Pacific Equatorial Undercurrent West of the Galápagos Archipelago
dc.type	Journal Paper
dc.journal.volume	52
dc.journal.issue	8
dc.journal.title	Journal of Physical Oceanography
dc.identifier.doi	10.1175/JPO-D-21-0124.1
dc.journal.fristpage	1927
dc.journal.lastpage	1943
dc.page	1927–1943
dc.tree	Journal of Physical Oceanography:;2022:;volume( 052 ):;issue: 008
dc.contenttype	Fulltext