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搜索结果: 1-10 共查到理学 Indonesian Throughflow相关记录10条 . 查询时间(0.14 秒)
In the summer of 1954, I accepted a position as an oceanographer at the Marine Science Institute in Djakarta, Indonesia. When I arrived in November 1954, I found out that all the Dutch scientists had ...
The relatively intense boundary currents of the western equatorial Pacific, as well as the western Pacific warm pool, have long been recognized as key components in the global climate system. More rec...
A simple analytical model of the closure of the wind-driven gyres in the tropical west Pacific is developed to illustrate the role of Halmahera and variations in the Pacific wind stress on the water m...
Godfrey's Island Rule is rederived in terms of the barotrapic streamfunction for flow in a stratified ocean with a rigid lid. Modifications to include bottom topography and frictional effects along ea...
Most available wind products show a mean wind stress curl across the Pacific atN that is close to zero, so a Sverdrup model predicts the western boundary current at the Asian coast to be nearly zer...
The effect of the Indonesian Throughflow on the World Ocean circulation is examined by a series of experiments with a global ocean GCM. The principal objective is to gain an understanding of how ocean...
The timescale and mechanisms of remote response in a global ocean GCM is investigated in the case of a sudden change in the rate of Indonesian Throughflow. In one experiment, the model is run to equil...
South of Tasmania, the Fine Resolution Antarctic Model (FRAM) shows a narrow band of westward flow in the surface layer. The authors argue that this is caused by the closure of the Indonesian passage ...
The near-surface dynamics and thermodynamics of the Indian Ocean are examined in a global ocean general circulation model (OGCM) with enhanced tropical resolution. The model uses a Seager-type heat fl...
Effects of the Indonesian Throughflow (ITF) on the circulation and thermal structure of the Pacific and Indian Oceans are studied by comparing solutions of a near-global ocean general circulation mode...

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