摘要
本文利用牛顿力学基本原理定性和定量地初步分析了海洋的潮汐现象.海洋的潮汐现象基本来自月球的引力作用,在较小程度上也来自太阳的引力作用.潮汐产生力决定于引力的梯度,据此给出了潮汐产生力的全貌,估算了在开阔海面处潮的平均高度,讨论了太阳引力的影响及大潮小潮等问题.
the articale initially analyzes ocean tide phenomenon qualitatively and quantitatively by the principal law of Newton's mechanics.The tide phenomenon of the ocean is produced by the gravitation of the moon,at smaller extent,also by the gravitation of the sun.The tidal force decides gradient of gravitation,according to this,tide force of full view is gained. The usual height of the tide can be calculated at the broad sea surface.Still talking about the influence of the sun and high,low tide question and so on.
出处
《北京机械工业学院学报》
1994年第1期110-116,共7页
Journal of Beijing Institute of Machinery
关键词
万有引力定律
惯性力
海洋
潮汐
The Law of Universal Gravitation
Inertial Force
The Gradient of Gravitation