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- W2098059511 abstract "Abstract A simple three-dimensional thermodynamic model is used to study the heat balance in the Gulf Stream region (30°–45°N, 40°–75°W) during the period from November 1992 to December 1999. The model is forced by surface heat fluxes derived from NCEP variables, with geostrophic surface velocity specified from sea surface height measurements from the TOPEX/Poseidon altimeter and Ekman transport specified from NCEP wind stress. The mixed layer temperature and mixed layer depth from the model show good agreement with the observations on seasonal and interannual time scales. Although the annual cycle of the upper-ocean heat content is underestimated, the agreement of the interannual variations in the heat content and the sea surface height are good; both are dominated by the large decrease from 1994 to 1997 and the increase afterward. As expected from previous studies, the surface heat flux dominates the seasonal and interannual variations in the mixed layer temperature. However, interannual variations in t..." @default.
- W2098059511 created "2016-06-24" @default.
- W2098059511 creator A5054541684 @default.
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- W2098059511 date "2004-05-01" @default.
- W2098059511 modified "2023-10-02" @default.
- W2098059511 title "Heat Budget in the Gulf Stream Region: The Importance of Heat Storage and Advection" @default.
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- W2098059511 doi "https://doi.org/10.1175/1520-0485(2004)034<1214:hbitgs>2.0.co;2" @default.
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