Features of the horizontal variability of the sea surface temperature in the Western Black Sea from high resolution modeling


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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.

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A. Mizyuk

Marine Hydrophysical Institute; Moscow State University, Sevastopol Branch

编辑信件的主要联系方式.
Email: artem.mizyuk@yandex.ru
俄罗斯联邦, ul. Kapitanskaya 2, Sevastopol’, 299011; ul. Geroev Sevastopolya 7, Sevastopol’, 299001

M. Senderov

Marine Hydrophysical Institute

Email: artem.mizyuk@yandex.ru
俄罗斯联邦, ul. Kapitanskaya 2, Sevastopol’, 299011

G. Korotaev

Marine Hydrophysical Institute

Email: artem.mizyuk@yandex.ru
俄罗斯联邦, ul. Kapitanskaya 2, Sevastopol’, 299011

A. Sarkysyan

Institute of Numerical Mathematics

Email: artem.mizyuk@yandex.ru
俄罗斯联邦, ul. Gubkina 8, Moscow, 119333

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