The Secondary Sea Level Maximum during Floods in Saint Petersburg and Its Simulation with Numerical Models
- Authors: Popov S.K.1, Gusev A.V.2,3, Fomin V.V.4
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Affiliations:
- Hydrometeorological Research Center of the Russian Federation
- Marchuk Institute of Numerical Mathematics
- Shirshov Institute of Oceanology
- Zubov State Oceanographic Institute
- Issue: Vol 43, No 12 (2018)
- Pages: 827-836
- Section: Article
- URL: https://journal-vniispk.ru/1068-3739/article/view/231309
- DOI: https://doi.org/10.3103/S1068373918120038
- ID: 231309
Cite item
Abstract
The study considered two- and three-dimensional models used to compute the Baltic Sea level. It is demonstrated for three floods that the BALT-P three-dimensional hydrodynamic model and the INMOM three-dimensional hydrothermodynamics model successfully simulate extreme sea level fluctuations during the floods in Saint Petersburg. To simulate extreme sea level fluctuations in the Baltic Sea, it is appropriate to use the BALT-P model which requires less input information. The analysis of simulation data for the considered cases reveals that the reason for the occurrence of the second flood maximum is the excitation of the wind-induced fundamental single-node seiche of the Baltic Sea.
About the authors
S. K. Popov
Hydrometeorological Research Center of the Russian Federation
Author for correspondence.
Email: lmpi@yandex.ru
Russian Federation, Bolshoi Predtechenskii per. 11–13, Moscow, 123242
A. V. Gusev
Marchuk Institute of Numerical Mathematics; Shirshov Institute of Oceanology
Email: lmpi@yandex.ru
Russian Federation, ul. Gubkina 8, Moscow, 119333; Nakhimovskii pr. 36, Moscow, 117997
V. V. Fomin
Zubov State Oceanographic Institute
Email: lmpi@yandex.ru
Russian Federation, Kropotkinskii per. 6, Moscow, 119034
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