The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is also shown that the large-scale wind cannot directly affect the aspg. However, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 134.95 Kb. 2
The origin of along-shelf pressure gradient in the Middle Atlantic Bight Cape Hatteras. It is shown that the large-scale wind pattern cannot directly affect the aspg. On the other hand, north of the Gulf Stream, there exist seasonal and inter-annual variations of eddy kinetic energy which affect the aspg 74.87 Kb. 1
Variability of the Oceanic Mixed Layer 1960-2004 Sst, suggesting that other processes such as advection are more important. Interestingly, at decadal periods the winter-spring mixed layers of both basins show trends, deepening by 10-40m over the 45-year period of this analysis 0.7 Mb. 10