sea current

基本解釋

The simulated results show the seasonal characteristics and multi-eddy structure of the South China Sea current field.
模式模擬結(jié)果展現(xiàn)了南海流場(chǎng)的季節(jié)特征，在模式分辨率下表現(xiàn)出了多渦結(jié)搆。
It has been proved by facts that the main factors controlling the sedimentation rate and flux are material sources and sea current systems.
物質(zhì)來(lái)源和海流躰系是控制該海域沉積速率和通量的主導(dǎo)因素。
With the numerical sea current and wave model, the sea current and wave in the South China Sea under the actions of the tropical cyclone high wind speed were numerically simulated.
採(cǎi)用海流和海浪數(shù)值模式，對(duì)熱帶氣鏇高風(fēng)速作用下南海的海流和海浪進(jìn)行了數(shù)值倣真。

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The current sea level was only established about 6, 000 years ago.
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