Features of the horizontal variability of the sea surface temperature in the Western Black Sea from high resolution modeling
- Авторы: Mizyuk A.I.1,2, Senderov M.V.1, Korotaev G.K.1, Sarkysyan A.S.3
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Учреждения:
- Marine Hydrophysical Institute
- Moscow State University, Sevastopol Branch
- Institute of Numerical Mathematics
- Выпуск: Том 52, № 5 (2016)
- Страницы: 570-578
- Раздел: Article
- URL: https://journals.rcsi.science/0001-4338/article/view/148463
- DOI: https://doi.org/10.1134/S0001433816050108
- ID: 148463
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Аннотация
A parallel version of the NEMO complex ocean circulation model has been implemented for the Black Sea basin; the results of circulation numerical modeling with a high spatial resolution are presented. Analysis of the spatial variability is performed for the reconstructed hydrophysical fields in 2005–2008. The resulting simulated spatial variability characteristics of the sea surface temperature are compared with available satellite observational data.
Об авторах
A. Mizyuk
Marine Hydrophysical Institute; Moscow State University, Sevastopol Branch
Автор, ответственный за переписку.
Email: artem.mizyuk@yandex.ru
Россия, ul. Kapitanskaya 2, Sevastopol’, 299011; ul. Geroev Sevastopolya 7, Sevastopol’, 299001
M. Senderov
Marine Hydrophysical Institute
Email: artem.mizyuk@yandex.ru
Россия, ul. Kapitanskaya 2, Sevastopol’, 299011
G. Korotaev
Marine Hydrophysical Institute
Email: artem.mizyuk@yandex.ru
Россия, ul. Kapitanskaya 2, Sevastopol’, 299011
A. Sarkysyan
Institute of Numerical Mathematics
Email: artem.mizyuk@yandex.ru
Россия, ul. Gubkina 8, Moscow, 119333
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