Art

J-GLOBAL ID：201302283954404893   Reference number：13A1339994

Remotely induced warming of Antarctic Bottom Water in the eastern Weddell gyre

東部ウェッデル還流における南極底層水の遠方起源昇温

Author (11)： COULDREY Matthew P. (Univ. Southampton, Southampton, GBR) ,  JULLION Loiec (Univ. Southampton, Southampton, GBR) ,  JULLION Loiec (Florida State Univ., Florida, USA) ,  NAVEIRA GARABATO Alberto C. (Univ. Southampton, Southampton, GBR) ,  RYE Craig (Univ. Southampton, Southampton, GBR) ,  HERRAIZ-BORREGUERO Laura (Univ. Tasmania, Tasmania, AUT) ,  BROWN Peter J. (Univ. East Anglia, Norwich, GBR) ,  BROWN Peter J. (British Antarctic, Survey, Cambridge, GBR) ,  MEREDITH Michael P. (British Antarctic, Survey, Cambridge, GBR) ,  MEREDITH Michael P. (Scottish Assoc. Marine Sci., Oban, GBR) ,  SPEER Kevin L. (Florida State Univ., Florida, USA)
Material： Geophysical Research Letters  (Geophys Res Lett)
Volume： 40  Issue： 11  Page： 2755-2760  Publication year： Jun. 16, 2013 
JST Material Number： H0609B  ISSN： 0094-8276  Document type： Article
Article type： 短報  Country of issue： United States (USA)  Language： ENGLISH (EN)

Thesaurus term： *Antarctic Sea ,  gyre ,  *deep water ,  sea water temperature ,  Salinity ,  sea water density ,  T-S curve ,  tracer method ,  secular variation ,  oceanographic observation ,  fron ,  CTD observation ,  Weddell Sea ,  *Antarctic bottom water ,  Antarctic circumpolar current
Semi thesaurus term： South Pole circumpolar current ,  Southern Ocean

JST classification (1)： Structure and dynamics of ocean,circulation  (DC06030G)

Substance index (1)： CFC-11

Terms in the title (4)： 還流 ,  南極底層水 ,  起源 ,  昇温