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Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea : Особенности подхода к расчету режима волнения Каспийского моря. / Lopatukhin, L. I.; Yaitskaya, N. A.

в: Russian Meteorology and Hydrology, Том 43, № 4, 01.04.2018, стр. 245-250.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Lopatukhin, LI & Yaitskaya, NA 2018, 'Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea: Особенности подхода к расчету режима волнения Каспийского моря', Russian Meteorology and Hydrology, Том. 43, № 4, стр. 245-250. https://doi.org/10.3103/S1068373918040052

APA

Lopatukhin, L. I., & Yaitskaya, N. A. (2018). Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea: Особенности подхода к расчету режима волнения Каспийского моря. Russian Meteorology and Hydrology, 43(4), 245-250. https://doi.org/10.3103/S1068373918040052

Vancouver

Lopatukhin LI, Yaitskaya NA. Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea: Особенности подхода к расчету режима волнения Каспийского моря. Russian Meteorology and Hydrology. 2018 Апр. 1;43(4):245-250. https://doi.org/10.3103/S1068373918040052

Author

Lopatukhin, L. I. ; Yaitskaya, N. A. / Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea : Особенности подхода к расчету режима волнения Каспийского моря. в: Russian Meteorology and Hydrology. 2018 ; Том 43, № 4. стр. 245-250.

BibTeX

@article{6ec3a5e6dc624861b72b57bda1db1e35,
title = "Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea: Особенности подхода к расчету режима волнения Каспийского моря",
abstract = "A high-precision digital elevation model of the Caspian Sea with the spatial resolution of 0.001° x 0.001° is constructed and used as a basis for computation grids of various scales. A three-level scheme for calculating wind waves with the sequence of nested grids (Caspian Sea-Northern Caspian, Absheron Peninsula, Turkmenbashy city-the Northern Caspian key areas) is developed. A scenario designer is implemented which considers in calculations the ice edge position and the coastline dynamics. The SWAN spectral wave model is adapted to the Caspian Sea conditions. The series of calculations and the comparison of the obtained results with observational data are provided. It is found that the best result is obtained when corrected reanalysis data are used for calculations.",
keywords = "hydrodynamic model, model adaptation, The Caspian Sea, wind waves",
author = "Lopatukhin, {L. I.} and Yaitskaya, {N. A.}",
note = "Publisher Copyright: {\textcopyright} 2018, Allerton Press, Inc.",
year = "2018",
month = apr,
day = "1",
doi = "10.3103/S1068373918040052",
language = "English",
volume = "43",
pages = "245--250",
journal = "Russian Meteorology and Hydrology",
issn = "1068-3739",
publisher = "Allerton Press, Inc.",
number = "4",

}

RIS

TY - JOUR

T1 - Peculiarities of the Approach to Calculation of Wind Waves in the Caspian Sea

T2 - Особенности подхода к расчету режима волнения Каспийского моря

AU - Lopatukhin, L. I.

AU - Yaitskaya, N. A.

N1 - Publisher Copyright: © 2018, Allerton Press, Inc.

PY - 2018/4/1

Y1 - 2018/4/1

N2 - A high-precision digital elevation model of the Caspian Sea with the spatial resolution of 0.001° x 0.001° is constructed and used as a basis for computation grids of various scales. A three-level scheme for calculating wind waves with the sequence of nested grids (Caspian Sea-Northern Caspian, Absheron Peninsula, Turkmenbashy city-the Northern Caspian key areas) is developed. A scenario designer is implemented which considers in calculations the ice edge position and the coastline dynamics. The SWAN spectral wave model is adapted to the Caspian Sea conditions. The series of calculations and the comparison of the obtained results with observational data are provided. It is found that the best result is obtained when corrected reanalysis data are used for calculations.

AB - A high-precision digital elevation model of the Caspian Sea with the spatial resolution of 0.001° x 0.001° is constructed and used as a basis for computation grids of various scales. A three-level scheme for calculating wind waves with the sequence of nested grids (Caspian Sea-Northern Caspian, Absheron Peninsula, Turkmenbashy city-the Northern Caspian key areas) is developed. A scenario designer is implemented which considers in calculations the ice edge position and the coastline dynamics. The SWAN spectral wave model is adapted to the Caspian Sea conditions. The series of calculations and the comparison of the obtained results with observational data are provided. It is found that the best result is obtained when corrected reanalysis data are used for calculations.

KW - hydrodynamic model

KW - model adaptation

KW - The Caspian Sea

KW - wind waves

UR - http://www.scopus.com/inward/record.url?scp=85047514953&partnerID=8YFLogxK

U2 - 10.3103/S1068373918040052

DO - 10.3103/S1068373918040052

M3 - Article

AN - SCOPUS:85047514953

VL - 43

SP - 245

EP - 250

JO - Russian Meteorology and Hydrology

JF - Russian Meteorology and Hydrology

SN - 1068-3739

IS - 4

ER -

ID: 100951249