mirage

Halocline structure in the Canada Basin of the Arctic Ocean

WHOAS at MBLWHOI Library

a service of the MBLWHOI Library | About WHOAS

Show simple item record

dc.contributor.author Shimada, Koji
dc.contributor.author Itoh, Motoyo
dc.contributor.author Nishino, Shigeto
dc.contributor.author McLaughlin, Fiona A.
dc.contributor.author Carmack, Eddy
dc.contributor.author Proshutinsky, Andrey
dc.date.accessioned 2010-04-26T17:52:18Z
dc.date.available 2010-04-26T17:52:18Z
dc.date.issued 2005-02-05
dc.identifier.citation Geophysical Research Letters 32 (2005): L03605 en_US
dc.identifier.uri http://hdl.handle.net/1912/3318
dc.description Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 32 (2005): L03605, doi:10.1029/2004GL021358. en_US
dc.description.abstract We examine the varieties and spatial distributions of Pacific and Eastern Arctic origin halocline waters in the Canada Basin using 2002–2003 hydrographic data. The halocline structure in the Canada Basin is different from the Eastern Arctic halocline because it includes fresher Pacific Winter Waters that form a “cold halostad” which lies above the Eastern Arctic origin lower halocline waters. The structure of the halostad in the Canada Basin, however, is not spatially uniform, and depends on the pathway and history of the source water. Pacific Winter Water entering through the Bering Strait becomes salty due to sea ice formation and this, in turn, is dependent on the occurrence and distribution of polynyas. In particular, saline water from the eastern Chukchi Sea forms thick halostad and causes depression of the isohalines in the southern Canada Basin. This depression influences thermohaline structure of the oceanic Beaufort Gyre. en_US
dc.description.sponsorship This work was funded in part by the Japan Agency for Marine-Earth Science and Technology, the Fisheries and Oceans Canada, and the U.S. National Science Foundation. en_US
dc.format.mimetype application/pdf
dc.language.iso en_US en_US
dc.publisher American Geophysical Union en_US
dc.relation.uri http://dx.doi.org/10.1029/2004GL021358
dc.title Halocline structure in the Canada Basin of the Arctic Ocean en_US
dc.type Article en_US
dc.identifier.doi 10.1029/2004GL021358


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search WHOAS


Browse

My Account

Statistics