The origin of along-shelf pressure gradient in the Middle Atlantic BightThe origin of along-shelf pressure gradient in the Middle Atlantic Bight
Mab, and they produce sea surface sloping down to the north when they move further south. The influence of large-scale wind pattern on aspg is also examined
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A kq2a: What is the pattern of air movement in the troposphere? Variations in global insolationA kq2a: What is the pattern of air movement in the troposphere? Variations in global insolation
The tilt of the Earth's axis coupled with latitude controls the amount of insolation the Earth's surface receives. The higher the latitude the greater the seasonal variation of insolation
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The origin of along-shelf pressure gradient in the Middle Atlantic BightThe 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
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Tropical Atlantic Biases in ccsm4Tropical 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
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Precipitation from African Easterly WavesPrecipitation 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
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Akintunde mutairu oyewaleAkintunde mutairu oyewale
On forecasting malaria infection using autoregressive integrated moving average (arima) models
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