cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage

The Southern Ocean is especially sensitive to climate change, responding to winds that have increased over the past 30 years (Thompson and Solomon, 2002) and warming at about one degree per century in the core of the Antarctic Circumpolar Current (ACC; Gille, 2002). Drake Passage is a major control...

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Main Authors: Teresa K. Chereskin, D. Randolph Watts, Kathleen A. Donohue
Format: Article
Language:English
Published: The Oceanography Society 2012-09-01
Series:Oceanography
Subjects:
Online Access:http://tos.org/oceanography/archive/25-3_chereskin.pdf
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author Teresa K. Chereskin
D. Randolph Watts
Kathleen A. Donohue
author_facet Teresa K. Chereskin
D. Randolph Watts
Kathleen A. Donohue
author_sort Teresa K. Chereskin
collection DOAJ
description The Southern Ocean is especially sensitive to climate change, responding to winds that have increased over the past 30 years (Thompson and Solomon, 2002) and warming at about one degree per century in the core of the Antarctic Circumpolar Current (ACC; Gille, 2002). Drake Passage is a major control point of the ACC. It is a region of high mesoscale variability and complex topography. Eddies are thought to be essential for transferring momentum from the circumpolar winds that drive the ACC down to the seafloor where topographic form stresses regulate its transport. The cDrake experiment was designed to address fundamental dynamics not yet understood regarding wind forcing, eddy-mean momentum, and heat exchange, as well as form-drag interaction with bathymetry (Chereskin et al., 2009; http://cDrake.org).
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spelling doaj.art-75c1e079e6b64c45916e800028b7be552022-12-22T02:14:51ZengThe Oceanography SocietyOceanography1042-82752012-09-01253134135cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake PassageTeresa K. ChereskinD. Randolph WattsKathleen A. DonohueThe Southern Ocean is especially sensitive to climate change, responding to winds that have increased over the past 30 years (Thompson and Solomon, 2002) and warming at about one degree per century in the core of the Antarctic Circumpolar Current (ACC; Gille, 2002). Drake Passage is a major control point of the ACC. It is a region of high mesoscale variability and complex topography. Eddies are thought to be essential for transferring momentum from the circumpolar winds that drive the ACC down to the seafloor where topographic form stresses regulate its transport. The cDrake experiment was designed to address fundamental dynamics not yet understood regarding wind forcing, eddy-mean momentum, and heat exchange, as well as form-drag interaction with bathymetry (Chereskin et al., 2009; http://cDrake.org).http://tos.org/oceanography/archive/25-3_chereskin.pdfSouthern OceanDrake PassageAntarctic Circumpolar Current
spellingShingle Teresa K. Chereskin
D. Randolph Watts
Kathleen A. Donohue
cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
Oceanography
Southern Ocean
Drake Passage
Antarctic Circumpolar Current
title cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
title_full cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
title_fullStr cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
title_full_unstemmed cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
title_short cDrake: Dynamics and Transport of the Antarctic Circumpolar Current in Drake Passage
title_sort cdrake dynamics and transport of the antarctic circumpolar current in drake passage
topic Southern Ocean
Drake Passage
Antarctic Circumpolar Current
url http://tos.org/oceanography/archive/25-3_chereskin.pdf
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AT drandolphwatts cdrakedynamicsandtransportoftheantarcticcircumpolarcurrentindrakepassage
AT kathleenadonohue cdrakedynamicsandtransportoftheantarcticcircumpolarcurrentindrakepassage