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
Tropical Atlantic Biases in ccsm4 Abf a similar problem arises in the coupled model if the atmospheric component produces alongshore winds that are too weak. Erroneously warm coastal ssts spread westward through a combination of advection and positive air-sea feedback involving marine 1.09 Mb. 5
Precipitation from African Easterly Waves Itcz and its seasonal migration improves in the higher-resolution case. This suggests that capturing these transient waves and the resultant strong low-level convergence is one of the key ingredients for improving the simulation of precipitation in global 6.72 Mb. 4