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I. P. Medvedev

Researcher at Shirshov Institute of Oceanology

Publications -  47
Citations -  456

I. P. Medvedev is an academic researcher from Shirshov Institute of Oceanology. The author has contributed to research in topics: Sea level & Tide gauge. The author has an hindex of 9, co-authored 35 publications receiving 268 citations. Previous affiliations of I. P. Medvedev include Russian Academy of Sciences & Moscow State University.

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Tidal oscillations in the Baltic Sea

TL;DR: In this paper, the authors used long-term hourly data from 35 tide gauge stations, including 15 stations in the Gulf of Finland, to examine tidal sea level oscillations of the Baltic Sea.
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Tides in Three Enclosed Basins: The Baltic, Black, and Caspian Seas

TL;DR: In this article, the formation and predominance of diurnal or semidiurnal tides in these seas appears to depend on the frequency-selective properties of the basins and the diurnal radiational constituent S1 (1 cpd) was found to play an important role in general tidal dynamics.
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Acoustic-Gravity Lamb Waves from the Eruption of the Hunga-Tonga-Hunga-Hapai Volcano, Its Energy Release and Impact on Aerosol Concentrations and Tsunami

TL;DR: In this paper , the characteristics of acoustic gravity waves from the eruption of the Hunga-Tonga-Hunga-Hapai volcano detected at different infrasound stations of the Infrasound Monitoring System and at a network of low-frequency microbarographs in the Moscow region are studied.
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Variability of the Baltic Sea level and floods in the Gulf of Finland

TL;DR: In this paper, a cross spectral analysis of the synchronous observation series of the level in the Gulf of Finland has shown that the nodal lines of the standing dilatational waves are clearly traced with frequencies corresponding to the distance from the point of nodal line to the top of the gulf (a quarter of the wave length).
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Tides in the Black Sea: Observations and Numerical Modelling

TL;DR: In this paper, a numerical model of the Black Sea and adjacent Sea of Azov was developed and found to be in good agreement with tide gauge observations, and detailed tidal charts for amplitudes and phase lags of the major tidal harmonics in these two seas were constructed.