Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ. / Belonenko, T. V.; Bloshkina, E. V.; Makhotin, M. S.
в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том 2013, № 3, 2013, стр. 104-114.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
}
TY - JOUR
T1 - ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ
AU - Belonenko, T. V.
AU - Bloshkina, E. V.
AU - Makhotin, M. S.
N1 - Publisher Copyright: © 2013 Sankt-Petersburgskii Universitet. All rights reserved.
PY - 2013
Y1 - 2013
N2 - This study is based on NASA Physical Oceanography Distributed Active Archive Center's SST data daily taken for 2006-2010 years at nodes of a regular grid having discretion 0,08° . 0,08° in latitude and longitude. A dynamic-stochastic model of the sea surface temperature variation in the Japan Sea is used to assess the relative importance of different components such as zonal and meridian advections; horizontal turbulent heat flows; and heat flows on the air-water boundary. The greatest contribution to the SST variation is shown to have been made by heat flows on the air-water boundary, and the least one - by horizontal turbulent heat flow. The zonal advection contributes more than the meridian advection does. It is concluded that in 2010 there was a reverse of the components in terms of their contributions to the SST variability in the Japan Sea.
AB - This study is based on NASA Physical Oceanography Distributed Active Archive Center's SST data daily taken for 2006-2010 years at nodes of a regular grid having discretion 0,08° . 0,08° in latitude and longitude. A dynamic-stochastic model of the sea surface temperature variation in the Japan Sea is used to assess the relative importance of different components such as zonal and meridian advections; horizontal turbulent heat flows; and heat flows on the air-water boundary. The greatest contribution to the SST variation is shown to have been made by heat flows on the air-water boundary, and the least one - by horizontal turbulent heat flow. The zonal advection contributes more than the meridian advection does. It is concluded that in 2010 there was a reverse of the components in terms of their contributions to the SST variability in the Japan Sea.
KW - Dynamics-stochastic analysis
KW - Satellite data
KW - Sea surface temperature
KW - The Japan sea
UR - http://www.scopus.com/inward/record.url?scp=85044739996&partnerID=8YFLogxK
M3 - статья
VL - 2013
SP - 104
EP - 114
JO - Вестник Санкт-Петербургского университета. Науки о Земле
JF - Вестник Санкт-Петербургского университета. Науки о Земле
SN - 2541-9668
IS - 3
ER -
ID: 5636305