Author:
Ohashi Yoshihiko,Yamamoto-Kawai Michiyo,Kusahara Kazuya,Sasaki Ken’ichi,Ohshima Kay I.
Abstract
AbstractChlorofluorocarbon (CFC) and sulfur hexafluoride (SF6) were used to investigate the timescale of Antarctic Bottom Water (AABW) that spreads off Cape Darnley (CD) in East Antarctica. The age of the AABW was estimated based on the observed SF6/CFC-12 ratio while taking into account tracer dilution by Lower Circumpolar Deep Water. Along the western canyons off CD and the ~ 3000 to 3500 m isobaths, the bottom water age was < 5 years, reflecting the spread of newly formed CD Bottom Water. Higher ages of ~ 8 years obtained for areas east of CD and > 20 years in the northwestern offshore region indicate inflows of AABW through the Princess Elizabeth Trough and Weddell Sea Deep Water, respectively. This study determined the age distribution in the region off CD, where three different types of AABW spread.
Funder
Kurita Water and Environment Foundation
JSPS KAKENHI
Publisher
Springer Science and Business Media LLC
Cited by
4 articles.
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