Seiches in Petrozavodsk bay of the lake Onego

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Abstract

The analysis of observation data on fluctuations in the level and velocity of currents in the Petrozavodsk Bay of Lake Onega, performed in 2016–2017, was carried out. Level oscillations were measured with a discreteness of 10 s using two TDR-2050 devices (RBR Ltd., Canada). Spectral analysis was performed using the simple Fourier transform method after one-minute data averaging to reduce instrument noise. Energy-carrier periods corresponding to the seiches of Petrozavodsk Bay and the Lake Onega are identified. Current velocities were measured with Aquadopp HR-Profiler (Nortek, Norway). Within the framework of the linear long wave theory, seiche oscillations are considered in a model basin approximating the Petrozavodsk Bay with regard to the Ivanovskiye Islands. Using an analytical solution, estimates for the periods of the higher seiche modes and the corresponding maximum wave flow velocities are obtained for the Petrozavodsk Bay. The comparison of theoretical estimates with the data of field observations, was showed satisfactory agreement.

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About the authors

V. A. Ivanov

Marine Hydrophysical Institute RAS

Author for correspondence.
Email: uvmsev@yandex.ru
Russian Federation, 299009, Sevastopol

N. I. Pal’shin

Northern Water Problems Institute Karelian Research Center RAS

Email: uvmsev@yandex.ru
Russian Federation, 185030, Petrozavodsk

Yu. V. Manilyuk

Marine Hydrophysical Institute RAS

Email: uvmsev@yandex.ru
Russian Federation, 299009, Sevastopol

References

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Supplementary files

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2. Fig. 1. Map of the Petrozavodsk Bay and places of measurements of seiche oscillations: 1 - by the Valdai level recorders in 1964–1968, 2 - by the RCM current recorder in February 1987, 3 - comprehensive studies in March 2016 and 2017. I and II - the borders of the lip and Petrozavodsk Onego. The area marked with a rectangle in the right part of the picture corresponds to the left part of the picture.

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3. Fig. 2. Level fluctuations at the measurement station in Petrozavodsk Bay (a): 1 - March 2016, 2 - March 2017; spectral power density of level fluctuations (b).

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4. Fig. 3. Filtered level fluctuations in March 2017 with periods of 4 h 24 min (a), 1 h 20 min - 1 h 50 min (b), 31–36 min (c), 15–17 min (d), 8 –12 min (d) and 4–6 min (e).

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5. Fig. 4. Isolines of level (a), vector field of the flow velocity (b) of a single-node longitudinal seiche (k = 1, m = 0), τ10 = 32 min.

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6. Fig. 5. Isolines of level (a), vector field of the flow velocity (b) of a single-node transverse seiche (k = 0, m = 1), τ01 = 16 min.

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