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Sustained monitoring of the southern ocean at Drake Passage: Past achievements and future priorities

dc.contributor.authorMeredith, Michael P.
dc.contributor.authorWoodworth, Philip L.
dc.contributor.authorChereskin, Teresa K.
dc.contributor.authorMarshall, David P.
dc.contributor.authorAllison, Lesley C.
dc.contributor.authorBigg, Grant R.
dc.contributor.authorDonohue, Kathy
dc.contributor.authorHeywood, Karen J.
dc.contributor.authorHughes, Chris W.
dc.contributor.authorHibbert, Angela
dc.contributor.authorHogg, Andrew
dc.contributor.authorJohnson, Helen L.
dc.contributor.authorJullion, Loic
dc.contributor.authorKing, Brian A.
dc.contributor.authorLeach, Harry
dc.contributor.authorLenn, Yueng-Djern
dc.contributor.authorMaqueda, Miguel A Morales
dc.contributor.authorMunday, David R.
dc.contributor.authorGarabato, Albert C. Naveira
dc.contributor.authorProvost, Christine
dc.contributor.authorSallee, Jean-Baptiste
dc.contributor.authorSprintall, Janet
dc.date.accessioned2015-12-10T21:54:30Z
dc.date.issued2011
dc.date.updated2016-02-24T10:48:39Z
dc.description.abstractDrake Passage is the narrowest constriction of the Antarctic Circumpolar Current (ACC) in the Southern Ocean, with implications for global ocean circulation and climate. We review the long-term sustained monitoring programs that have been conducted at Drake Passage, dating back to the early part of the twentieth century. Attention is drawn to numerous breakthroughs that have been made from these programs, including (1) the first determinations of the complex ACC structure and early quantifications of its transport; (2) realization that the ACC transport is remarkably steady over interannual and longer periods, and a growing understanding of the processes responsible for this; (3) recognition of the role of coupled climate modes in dictating the horizontal transport and the role of anthropogenic processes in this; and (4) understanding of mechanisms driving changes in both the upper and lower limbs of the Southern Ocean overturning circulation and their impacts. It is argued that monitoring of this passage remains a high priority for oceanographic and climate research but that strategic improvements could be made concerning how this is conducted. In particular, long-term programs should concentrate on delivering quantifications of key variables of direct relevance to large-scale environmental issues: In this context, the time-varying overturning circulation is, if anything, even more compelling a target than the ACC flow. Further, there is a need for better international resource sharing and improved spatiotemporal coordination of the measurements. If achieved, the improvements in understanding of important climatic issues deriving from Drake Passage monitoring can be sustained into the future.
dc.identifier.issn8755-1209
dc.identifier.urihttp://hdl.handle.net/1885/38967
dc.publisherAmerican Geophysical Union
dc.rightsAuthor/s retain copyrighten_AU
dc.sourceReviews of Geophysics
dc.subjectKeywords: Antarctic circumpolar current; Anthropogenic process; Climate research; Drake passage; Environmental issues; Global ocean circulation; Horizontal transport; Interannual; International resources; Key variables; Lower limb; Monitoring programs; Overturning
dc.titleSustained monitoring of the southern ocean at Drake Passage: Past achievements and future priorities
dc.typeJournal article
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issueRG4005
local.bibliographicCitation.lastpage36
local.bibliographicCitation.startpage1
local.contributor.affiliationMeredith, Michael P., British Antarctic Survey
local.contributor.affiliationWoodworth, Philip L., National Oceanography Centre
local.contributor.affiliationChereskin, Teresa K., Scripps Institution of Oceanography
local.contributor.affiliationMarshall, David P., University of Oxford
local.contributor.affiliationAllison, Lesley C., University of Reading
local.contributor.affiliationBigg, Grant R., University of Sheffield
local.contributor.affiliationDonohue, Kathy, Univeristy of Rhode Island
local.contributor.affiliationHeywood, Karen J., University of East Anglia
local.contributor.affiliationHughes, Chris W., National Oceanography Centre
local.contributor.affiliationHibbert, Angela, University of Liverpool
local.contributor.affiliationHogg, Andrew, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationJohnson, Helen L., University of Oxford
local.contributor.affiliationJullion, Loic, National Oceanography Centre
local.contributor.affiliationKing, Brian A., National Oceanography Centre
local.contributor.affiliationLeach, Harry, University of Liverpool
local.contributor.affiliationLenn, Yueng-Djern, Bangor University
local.contributor.affiliationMaqueda, Miguel A Morales, National Oceanography Centre
local.contributor.affiliationMunday, David R., University of Oxford
local.contributor.affiliationGarabato, Albert C. Naveira, National Oceanography Centre
local.contributor.affiliationProvost, Christine, Universite Pierre et Marie Curie
local.contributor.affiliationSallee, Jean-Baptiste, British Antarctic Survey
local.contributor.affiliationSprintall, Janet, Scripps Intitution of Oceanography
local.contributor.authoruidHogg, Andrew, u3586031
local.description.notesImported from ARIES
local.identifier.absfor040104 - Climate Change Processes
local.identifier.absfor040503 - Physical Oceanography
local.identifier.absseo960303 - Climate Change Models
local.identifier.absseo961104 - Physical and Chemical Conditions of Water in Marine Environments
local.identifier.ariespublicationu4278572xPUB169
local.identifier.citationvolume49
local.identifier.doi10.1029/2010RG000348
local.identifier.scopusID2-s2.0-82955177009
local.identifier.thomsonID000297677100001
local.type.statusPublished Version

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