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Large-Scale SST Variability in the Western North Atlantic Subtropical Convergence Zone during FASINEX. Part II：Upper Ocean Heat Balance and Frontogenesis
subtropical frontal zone sea surface temperature Upper Ocean Heat Balance Frontogenesis
2008/12/27
We analyzed the influence of wind-deriven horizontal heat advection on the large-scale [O(1000) km wavelength] variability of both the upper-ocean mixed-layer heat content and the subtropical frontal ...
Upper-Ocean Heat Balance in the Kuroshio Extension Region
Upper-Ocean Heat Balance Kuroshio Extension Region two-dimensional mixed-layer model
2008/12/19
A horizontally two-dimensional mixed-layer model is used to study the upper-ocean heat balance in the Kuroshio Extension region (30°–40°N, 141°–175°E). Horizontal dependency is emphasized because, in ...
Heat Flux Estimates for the Western North Atlantic. Part II：The Upper-Ocean Heat Balance
Upper-Ocean Heat Balance Western North Atlantic Heat Flux
2008/12/12
The assimilation of temperature and altimetric velocity into a numerical model of the upper-ocean mixed layer in Part I allowed an analysis of the upper ocean heat budget for the western North Atlanti...