表面风是控制非潮汐的海流表面浪的基本营力。
The surface wind is the principal agent controlling nontidal currents 'surface waves.
在综合分析的基础上，进一步建立了该区水道型和非水道型内波内潮汐沉积模式。
Finally, the inter wave and inter tide sedimentary model of channels and non channels has been established on the basis of comprehensive analysis.
基于全球海洋数值模式，估计了海水质量非潮汐变化对低阶地球引力场季节性变化的贡献。
Based on the global numerical ocean models, the contributions of nontidal oceanic mass change to the seasonal variations in the low-degree Earth's gravitational field are estimated.
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