Email this article Features of the horizontal variability of the sea surface temperature in the Western Black Sea from high resolution modeling
- Authors: Mizyuk A.I.1,2, Senderov M.V.1, Korotaev G.K.1, Sarkysyan A.S.3
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Affiliations:
- Marine Hydrophysical Institute
- Moscow State University, Sevastopol Branch
- Institute of Numerical Mathematics
- Issue: Vol 52, No 5 (2016)
- Pages: 570-578
- Section: Article
- URL: https://journal-vniispk.ru/0001-4338/article/view/148463
- DOI: https://doi.org/10.1134/S0001433816050108
- ID: 148463
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Abstract
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.
About the authors
A. I. Mizyuk
Marine Hydrophysical Institute; Moscow State University, Sevastopol Branch
Author for correspondence.
Email: artem.mizyuk@yandex.ru
Russian Federation, ul. Kapitanskaya 2, Sevastopol’, 299011; ul. Geroev Sevastopolya 7, Sevastopol’, 299001
M. V. Senderov
Marine Hydrophysical Institute
Email: artem.mizyuk@yandex.ru
Russian Federation, ul. Kapitanskaya 2, Sevastopol’, 299011
G. K. Korotaev
Marine Hydrophysical Institute
Email: artem.mizyuk@yandex.ru
Russian Federation, ul. Kapitanskaya 2, Sevastopol’, 299011
A. S. Sarkysyan
Institute of Numerical Mathematics
Email: artem.mizyuk@yandex.ru
Russian Federation, ul. Gubkina 8, Moscow, 119333
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