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The evolution of upper ocean thermal structure at 10⁰N, 125⁰W during 1997-1998
(Massachusetts Institute of Technology, 2003)
In this thesis I have endeavored to determine the factors and physical processes that controlled SST and thermocline depth at 10⁰N, 125⁰W during the Pan Amer- ican Climate Study (PACS) field program. Analysis based on the ...