Intrusion of Circumpolar Deep Water over the continental shelf in the central Amundsen Sea.
Cited 0 time in
Cited 0 time in
-
Title
-
Intrusion of Circumpolar Deep Water over the continental shelf in the central Amundsen Sea.
-
Other Titles
-
아문젠해역으로 유입되는 남극순환류.
-
Authors
-
Kim, Tae-Wan
A. Wahlin
K.W. Nicholls
Lee, Sang H.
Lee, Jae-Hak
Ha, Ho Kyung
-
Keywords
-
Amundsen Sea; Circumpolar Deep water
-
Issue Date
-
2012
-
Citation
-
Kim, Tae-Wan, et al. 2012. Intrusion of Circumpolar Deep Water over the continental shelf in the central Amundsen Sea.. Filchner Ronne Ice Shelf Programme(FRISP). Filchner Ronne Ice Shelf Programme(FRISP). 2012.11.23~.
-
Abstract
-
The Amundsen Sea sector is the most rapidly changing region of the Antarctic ice sheets. It has
been claimed that the rapid retreat of the glaciers (or ice sheets) is primarily related to the
intrusion of warm Circumpolar Deep Water (CDW) which acts as an oceanic heat source. The Amundsen
shelf troughs were suspected to be main conduits supplying warm CDW onto the continental shelf,
eroding the underside of the ice sheets and glaciers.
Despite the critical role of CDW in the continental shelf of the Amundsen Sea, vital information
is still lacking concerning the spatial-temporal variability of CDW. This is mainly because the
Amundsen Sea is remotely located and the harsh weather and sea conditions limit the access to its
inner shelf. This pronounced lack of data hinders the evaluation and prediction of physical
processes and associated biogeochemicalprocesses in the Amundsen Sea.
Using the icebreaker R/V Araon, three institutes (KOPRI,UGOT and BAS) launched a resource-sharing
program for monitoring the distribution of CDW and associated rapid melting of glaciers in the
Amundsen Shelf. During the 2012 Amundsen Sea cruise, 52 CTD stations were visited, and a total of
6 moorings were successfully recovered and 15 moorings were newly deployed at the shelf break,
troughs and ice shelf front. During the presentation, preliminary data and results archived during
the 2012 Araon cruise will be pr) which acts as an oceanic heat source. The Amundsen
shelf troughs were suspected to be main conduits supplying warm CDW onto the continental shelf,
eroding the underside of the ice sheets and glaciers.
Despite the critical role of CDW in the continental shelf of the Amundsen Sea, vital information
is still lacking concerning the spatial-temporal variability of CDW. This is mainly because the
Amundsen Sea is remotely located and the harsh weather and sea conditions limit the access to its
inner shelf. This pronounced lack of data hinders the
-
URI
-
https://repository.kopri.re.kr/handle/201206/8390
-
Conference Name
-
Filchner Ronne Ice Shelf Programme(FRISP)
-
Conference Place
-
Filchner Ronne Ice Shelf Programme(FRISP)
-
Conference Date
-
2012.11.23~
-
Type
-
Proceeding
-
Indexed
-
Pro(초록)국외
- Appears in Collections
- 2012-2013, Physical & Bio-geochemical Processes in the Polar Sea Ice Regions: Their Roles & Responses in Global Climate Change (12-13) / Lee, Sang H. (PP12010; PP13020)
- Files in This Item
-
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.