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static theory of tides
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static theory of tides
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理学
潮汐静力学理论
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static theory of tides
潮汐静力学理论
假设地球为均一水深的水球,并能够对天体引潮力的作用迅速响应,忽略陆地分布、底地形、摩擦与惯性效应的影响,在各力的作用下海水不断达到新的平衡位置,从而引起海表面水位的周期性变化。又称平衡潮理论。
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