Abstract

A method for studying stamukhas using the modern field equipment is considered. The peculiarities of morphometric characteristics and parameters of the internal structure of stamukhas are analyzed. The interrelation between the consolidated layer thickness and the accumulated freezing degree days is derived for different seas. The comparative analysis of morphometric characteristics and the consolidated layer in the ice-covered seas of Russia is carried out. It is shown that the formation of stamukhas in different regions has specific features depending on the depth, bottom topography, drift characteristics, ice thickness, and dates of fast ice formation. The maximum thickness of the consolidated layer is registered in the Kara and Laptev seas.

中文翻译：

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俄罗斯冰雪覆盖的海洋中Stamukhas的形态和内部结构

摘要

考虑了一种使用现代现场设备研究葡萄柚的方法。分析了stamukhas的形态特征和内部结构参数的特点。推导了不同海域固结层厚度与累积冰冻天数之间的相互关系。对俄罗斯冰雪覆盖海域的形态特征和固结层进行了对比分析。结果表明，取决于深度，底部地形，漂移特征，冰的厚度和快速形成冰的日期，不同地区的stamukhas形成具有特定的特征。固结层的最大厚度记录在卡拉海和拉普捷夫海中。