摘要
海洋内波生成及演变是内波研究的关键问题之一,人们对于海洋内波的生成机制的研究由来已久,无论是国内还是国外的研究人员都进行了大量的努力研究和探讨并取得了丰硕的成果。从海洋内波的生成机制来看,一般可以将其分为高频随机内波和低频的内潮波、内孤立波、惯性内波以及近惯性内波等。可以激发内波的生成源可能存在于在海面、海洋内部或者海底,对不同生成源,对应内波的生成机制也不同,该文介绍了不同位置的内波生成源及其生成机制。
Generation and evolution of ocean internal wave is one of the key problems in the studies of internal waves.The generation mechanism of internal waves in the ocean have been studied for a long time, both domestic and foreign researchers have been a large number of research efforts and explore and achieved fruitful results. From the point of view of the formation mechanism of internal waves in the ocean, generally can be divided for high frequency random internal waves and low frequency in the tidal wave, internal solitary waves, inertial waves and near inertial internal waves and so on. The source which can inspire the source for the generation of the internal waves may exist in the sea, the interior of the ocean or the bottom of the sea.As for different source, corresponding internal wave generation mechanism is also different. This paper introduces the source of internal waves generated at different positions and its formation mechanism.
出处
《科技创新导报》
2015年第35期186-187,共2页
Science and Technology Innovation Herald
关键词
海洋内波
生成源
生成机制
Tbe ocean waves
Generating source
Formation mechanism