Approach to solving the problem of sea level forecasting off Cape Kamenny in the Ob’ Bay

Author:

Voinov G. N.1,Golovin N. V.1,Kubyshkin N. V.2,Kulakov M. Yu.1,Skutin A. A.1,Smirnov K. G.1,Khaimina O. V.3

Affiliation:

1. State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute

2. “Arctic Shelf Consulting” LLC

3. Russian State Hydrometeorological University

Abstract

The problem of short-term sea level forecasting in the area of Сape Kamenny in the Ob’ Bay has become important since the Novoportovsky terminal (known as “Arctic Gate”) began operating for year-round oil shipment. The tankers loading the oil from the terminal have to pass through relatively shallow waters, located to the north, limiting the vessels draft. Thereby a short-term water level forecast is required relative to the lowest theoretical level for tankers loading at the terminal. The year-round hourly observations using buoy level gauges with a satellite channel of data transmission are organized for quick level monitoring directly in the area of Cape Kamenny. The results of the harmonic analysis of water level observations in the area of Cape Kamenny for 2016–2021 showed significant seasonal variability of amplitudes and phases of the wave М2 in the annual cycle, as well as their interannual variability due to various ice conditions of the Ob’ Bay (light, medium, heavy). Based on these results, the processing and analysis of observations data over the last month are performed by the end of each month. According to these results, the current values of harmonic constants, dependent on actual ice conditions are specified and calculation of the tide is carried out for the next month. The calculation of the forecast values of the total level is composed of calculated tide and short term (with a lead time of up to 5 days) forecast of non-periodic level fluctuations using the three-dimensional hydrodynamic model of joint water and ice circulation AARI-IOCM. At the final stage of the forecast preparation, the predicted level, usually calculated relative to the conditional long term average annual value, is bound to the lowest theoretical level (according to the current values of the level gauge) and transferred to the operator of the terminal and to the tanker. The hourly observations of water level in the area of Cape Kamenny and level forecasting have been carried out since 2017 and are still continuing.

Publisher

FSBI Arctic and Antarctic Research Institute (FSBI AARI)

Subject

General Medicine

Reference17 articles.

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2. Kopteva A.V. Level and currents of the Ob’ Bay. Trudy AANII. Proc. of AARI. 1953, 59: 84–148. [In Russian].

3. Kopteva A.V., Butenko A.K., Ivanova Z.K. Materials for the study of tides in the arctic seas of the USSR. Trudy AANII. Proc. of AARI. 1952, 42 (issue VII. Kara Sea): 536 p. [In Russian].

4. Diesperova R.A. Tides of the Arctic Ocean. Trudy GOIN. Proc. of GOIN. 1954, 19: 74 p. [In Russian].

5. Voinov G.N., Piskun A.A. Tidal and storm surges water level fluctuations at the Cape Kamenny area (Ob’ Bay). Problemy Arktiki i Antarktiki. Arctic and Antarctic Research. 2019, 1 (65): 15–33. [In Russian].

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