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Tides in the southern area of the Kara Sea in the vicinity of the Belyi island
Author(s) -
Г. Н. Войнов,
О. А. Морозова,
А. В. Нестеров,
Konstantin A. Kornishin,
Я. О. Ефимов
Publication year - 2020
Publication title -
problemy arktiki i antarktiki
Language(s) - English
Resource type - Journals
eISSN - 2618-6713
pISSN - 0555-2648
DOI - 10.30758/0555-2648-2020-66-1-6-19
Subject(s) - buoy , geology , geodesy , ridge , series (stratigraphy) , sea level , climatology , meteorology , oceanography , geography , paleontology
A number of promising hydrocarbon deposits are known in the south-western part of the Kara Sea. A safe development of these deposits requires hydrometeorological support, including sea-level observations. The paper deals with sea-level data of autonomous anchored buoy station. The period of observation is about 2 years, and the observation dataset is divided into 2 periods due to the displacement of the buoy station. The coordinates of the first position of the buoy station are known but they had been changed after the displacement (possibly due to the action of the ice ridge keels). Data from two time series of observations are studied by harmonic analysis, using the method of least squares by AARI version. According to the average monthly and mean annual values of the main tides it is found that the data includes two independent series. It is determined that the second series may be considered uniform. In order to locate of the anchored buoy station we calculated new coordinates using the empirical tidal charts of the M 2 wave. As a result, the harmonic constants of the eight main tidal waves for the Belyi Island area are presented for the first time. The new data confirms the amphidromic system in tides O 1 and Q 1 , between the Zhelaniya Cape and the Belyi Island. According to the new data the maximum seasonal variation in the range of M2 tide was observed in June, and the minimum of the phase angle was observed in July. This unusual seasonal variation of the M 2 tide corresponds to previous observations data from the Uedinenia Island. The authors have no competing interests.

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