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Record #32871:

Рельеф дна как основной фактор, формирующий незональность Антарктического циркумполярного течения

Title: Рельеф дна как основной фактор, формирующий незональность Антарктического циркумполярного течения
Title, transliterated: Relʹef dna kak osnovnoĭ faktor, formirui︠u︡shchiĭ nezonalʹnostʹ Antarkticheskogo t︠s︡irkumpoli︠a︡rnogo techenii︠a︡ / I︠U︡.A. Ivanov, V.M. Kamenkovich.
Translated title: Bottom topography as the main factor in forming the non-zonality of the Antarctic circumpolar current.
Author(s): Ivanov, I︠U︡. A.
Kamenkovich, V. M.
Date: 1959.
Language: Russian.
In: Doklady Akademii Nauk SSSR. (1959.), l28(6) (1959)
Abstract: The Antarctic circumpolar current has a relatively uniform vertical structure and penetrates as far as the bottom, so that the initial equations of Eklund's theory can be used for a theoretical model. Expressions are derived for determining the forms of the isolines of full flow; they are substantially created by the conjunction of latitudinal variations in the Coriolis force and by the bottom topography.
Notes:

Doklady Akademii Nauk SSSR. l28(6) :1l67-l170 (1959).

Keywords: 551.46 -- Oceanography, physical.
551.462 -- Submarine topography, bottom forms.
551.465.5 -- Ocean currents.
C -- Oceanography, hydrography and hydrology.
(*7) -- Antarctic regions.
(*80) -- Southern Ocean.
SPRI record no.: 32871

MARCXML

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001 SPRI-32871
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007 ta
008 240329s1959####xx#b##|##|###|0||#0|rus#d
035 ## ‡aSPRI-32871
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aIvanov, I︠U︡. A.
242 10 ‡aBottom topography as the main factor in forming the non-zonality of the Antarctic circumpolar current.‡yeng
245 10 ‡6880-02‡aRelʹef dna kak osnovnoĭ faktor, formirui︠u︡shchiĭ nezonalʹnostʹ Antarkticheskogo t︠s︡irkumpoli︠a︡rnogo techenii︠a︡ /‡cI︠U︡.A. Ivanov, V.M. Kamenkovich.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1959.
300 ## ‡ap. 1l67-l170 :‡bgraph, maps.
500 ## ‡aDoklady Akademii Nauk SSSR. l28(6) :1l67-l170 (1959).
520 3# ‡aThe Antarctic circumpolar current has a relatively uniform vertical structure and penetrates as far as the bottom, so that the initial equations of Eklund's theory can be used for a theoretical model. Expressions are derived for determining the forms of the isolines of full flow; they are substantially created by the conjunction of latitudinal variations in the Coriolis force and by the bottom topography.
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 ‡a551.462 -- Submarine topography, bottom forms.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
700 1# ‡6880-03‡aKamenkovich, V. M.
773 0# ‡6880-04‡7nnas ‡tDoklady Akademii Nauk SSSR. ‡gl28(6) (1959) ‡wSPRI-21027
880 1# ‡6100-01/(N‡aИванов, Ю. А.
880 10 ‡6245-02/(N‡aРельеф дна как основной фактор, формирующий незональность Антарктического циркумполярного течения /‡cЮ.А. Иванов, В.М. Каменкович.
880 1# ‡6700-03/(N‡aКаменкович, В. М.
880 0# ‡6773-04/(N‡7nnas ‡tДоклады Академии Наук СССР. ‡gl28(6) (1959) ‡wSPRI-21027
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329