The results of investigations into internal waves on a narrow steep shelf of the northeastern coast of the Black Sea are presented here. To measure the parameters of internal waves, the spatial antenna of three autonomous line temperature sensors were equipped in the depth range of 17 to 27 m. In observations that lasted for 10 days, near-inertial internal waves with a period close to 17 h and short-period internal waves with periods of 2–8 min, regularly approaching the coast, were revealed. The wave amplitudes were 4–8 m for inertial waves and 0.5–4 m for short-period internal waves. It was determined that most of the short-period internal waves approached from the southeast direction, from Cape Kodor. A large number of short waves reflected from the coast were also recorded. The intensification of short-period waves with inertial periodicity and the belonging of trains of short waves to crests of inertial waves were identified. In general, it was shown that the internal wave field at a narrow shelf significantly differs in its features from analogs of ordinary shelves of the Black Sea.

中文翻译：

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利用线温度传感器的空间天线研究黑海狭窄陡峭大陆架的内波

此处介绍了对黑海东北海岸狭窄陡峭陆架上的内部波浪的调查结果。为了测量内部波的参数，在17至27 m的深度范围内配备了三个自主线路温度传感器的空间天线。在持续了10天的观测中，发现定期接近海岸的近惯性内波（周期约17小时）和短周期内波（周期约2-8分钟）。惯性波的波幅为4-8 m，短周期内波的波幅为0.5-4 m。可以确定，大多数短周期内波是从东南方向（科多角角）接近的。还记录了从海岸反射的大量短波。确定了具有惯性周期性的短周期波的增强以及短波列属于惯性波波峰的原因。总的来说，已经表明，狭窄海域的内部波场在特征上与黑海普通海域的类似物有很大不同。