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Record #187467:

Гидрофизические характеристики придонного слоя глубоководных районов Арктического бассейна Северного Ледовитого океана

Title: Гидрофизические характеристики придонного слоя глубоководных районов Арктического бассейна Северного Ледовитого океана
Title, transliterated: Gidrofizicheskie kharakteristiki pridonnogo sloi︠a︡ glubokovodnykh raĭonov Arkticheskogo basseĭna Severnogo Ledovitogo okeana / I.E. Frolov, I.M. Ashik, V.T. Sokolov.
Translated title: Hydrophysical parameters of the near-bottom layer of deep water sections of the Arctic Basin.
Author(s): Frolov, I. E.
Ashik, I. M.
Sokolov, V. T.
Date: 2007.
Language: Russian.
In: Problemy Arktiki i Antarktiki. (2007.), Vol. 75 (2007)
Abstract: Presents new data on vertical distribution of hydrological characteristics of waters of central Arctic Basin based on results of research expedition in 2005. Analyses differences in water temperature at various points and concludes that most likely heat source for warm layer formation in Arctic deep waters is geothermal processes in depths of lithosphere.
Notes:

Problemy Arktiki i Antarktiki. Vol. 75 :35-42 (2007).

Keywords: 551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.14 -- Lithosphere.
C -- Oceanography, hydrography and hydrology.
(*60) -- Arctic Ocean and adjacent waters.
SPRI record no.: 187467

MARCXML

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040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aFrolov, I. E.
242 10 ‡aHydrophysical parameters of the near-bottom layer of deep water sections of the Arctic Basin.‡yeng
245 10 ‡6880-02‡aGidrofizicheskie kharakteristiki pridonnogo sloi︠a︡ glubokovodnykh raĭonov Arkticheskogo basseĭna Severnogo Ledovitogo okeana /‡cI.E. Frolov, I.M. Ashik, V.T. Sokolov.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2007.
300 ## ‡ap. 35-42 :‡bill., diags., tables.
500 ## ‡aProblemy Arktiki i Antarktiki. Vol. 75 :35-42 (2007).
520 3# ‡aPresents new data on vertical distribution of hydrological characteristics of waters of central Arctic Basin based on results of research expedition in 2005. Analyses differences in water temperature at various points and concludes that most likely heat source for warm layer formation in Arctic deep waters is geothermal processes in depths of lithosphere.
546 ## ‡aIn Russian.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.14 -- Lithosphere.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
700 1# ‡6880-03‡aAshik, I. M.
700 1# ‡6880-04‡aSokolov, V. T.
773 0# ‡6880-05‡7nnas ‡tProblemy Arktiki i Antarktiki. ‡gVol. 75 (2007) ‡wSPRI-14780
880 1# ‡6100-01/(N‡aФролов, И. Е.
880 10 ‡6245-02/(N‡aГидрофизические характеристики придонного слоя глубоководных районов Арктического бассейна Северного Ледовитого океана /‡cИ.Е. Фролов, И.М. Ашик, В.Т. Соколов.
880 1# ‡6700-03/(N‡aАшик, И. М.
880 1# ‡6700-04/(N‡aСоколов, В. Т.
880 0# ‡6773-05/(N‡7nnas ‡tПроблемы Арктики и Антарктики. ‡gVol. 75 (2007) ‡wSPRI-14780
916 ## ‡a2009/08/11 -- IW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924 ‡bIW