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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...