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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 изданияхстатьяРецензирование

Harvard

Belonenko, TV, Bloshkina, EV & Makhotin, MS 2013, 'ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том. 2013, № 3, стр. 104-114. <http://elibrary.ru/item.asp?id=21038929>

APA

Belonenko, T. V., Bloshkina, E. V., & Makhotin, M. S. (2013). ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2013(3), 104-114. http://elibrary.ru/item.asp?id=21038929

Vancouver

Belonenko TV, Bloshkina EV, Makhotin MS. ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2013;2013(3):104-114.

Author

Belonenko, T. V. ; Bloshkina, E. V. ; Makhotin, M. S. / ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ. в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2013 ; Том 2013, № 3. стр. 104-114.

BibTeX

@article{9a6905a270cc4d24961c9444302676be,
title = "ДИНАМИКО-СТОХАСТИЧЕСКАЯ МОДЕЛЬ ИЗМЕНЕНИЯ ТЕМПЕРАТУРЫ ПОВЕРХНОСТИ ЯПОНСКОГО МОРЯ ПО ДАННЫМ СПУТНИКОВЫХ ИЗМЕРЕНИЙ",
abstract = "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.",
keywords = "Dynamics-stochastic analysis, Satellite data, Sea surface temperature, The Japan sea",
author = "Belonenko, {T. V.} and Bloshkina, {E. V.} and Makhotin, {M. S.}",
note = "Publisher Copyright: {\textcopyright} 2013 Sankt-Petersburgskii Universitet. All rights reserved.",
year = "2013",
language = "русский",
volume = "2013",
pages = "104--114",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "3",

}

RIS

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