Short Internal Waves in a Small Ice-Covered Lake


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The high-precision observational data on water temperature obtained during seven winters in a small boreal lake are considered. The spectral analysis revealed that the oscillations with a period of about 27 min prevailed in a water column. This period is close to the theoretical estimate of the first mode of the longitudinal barotropic seiche. The variability of temperature oscillations, vertical velocity, and displacement of isotherms suggest the presence of short internal waves along with seiches. The amplitude of the internal waves is an order of magnitude greater than that of seiches, and the length of internal waves is two orders of magnitude less than the linear extent of the lake.

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N. Palshin

Northern Water Problems Institute

编辑信件的主要联系方式.
Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

S. Bogdanov

Northern Water Problems Institute

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

G. Zdorovennova

Northern Water Problems Institute

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

R. Zdorovennov

Northern Water Problems Institute

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

T. Efremova

Northern Water Problems Institute

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

B. Belashev

Institute of Geology

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185010

A. Terzhevik

Northern Water Problems Institute

Email: npalshin@mail.ru
俄罗斯联邦, Petrozavodsk, 185030

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