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Possible source of the antarctic bottom water in the Prydz Bay Region
Authors:Takashi Yabuki  Toshio Suga  Kimio Hanawa  Koji Matsuoka  Hiroshi Kiwada  Tomowo Watanabe
Institution:(1) Department of Geophysics, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan;(2) The Institute of Cetacean Research, Tokyo 104-0055, Japan;(3) National Research Institute of Fisheries Science, Yokohama 236-8648, Japan
Abstract:It has been inferred that the Prydz Bay region is one of the source regions of Antarctic Bottom Water (AABW) based on rather indirect evidence. In order to examine this inference, we investigate the hydrographic condition of the bay based mainly on XCTD data obtained during the Japanese Whale Research Program in the Antarctic (JARPA). The JARPA hydrographic data reveal Circumpolar Deep Water (CDW), which is a salty, warm water mass approaching the shelf break, and capture Modified CDW (MCDW) intruding into the shelf water. AABW production requires mixing of CDW and cold shelf water saltier than 34.6 psu, which is a saltier type of Low Salinity Shelf Water (LSSW). Saltier LSSW is observed near the bottom over the shelf, being mixed with MCDW. We further identify saltier LSSW near the shelf break. This saltier LSSW appears close enough to unmodified CDW to be mixed with it over the continental slope, indicating a possible source of AABW in Prydz Bay.
Keywords:Antarctic Bottom Water  Prydz Bay  Amery Basin  JARPA  Circumpolar Deep Water  Ice Shelf Water  XCTD  continental shelf  ice shelf
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