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Record #78015:

Объемный T, С-анализ водных масс антарктического происхождения в индийском секторе Южного океана

Title: Объемный T, С-анализ водных масс антарктического происхождения в индийском секторе Южного океана
Title, transliterated: Obʺemnyĭ T, S-analiz vodnykh mass antarkticheskogo proiskhozhdenii︠a︡ v indiĭskom sektore I︠U︡zhnogo okeana / A.T. Bozhkov, A.A. Dmitrieva, A.V. Menʹshenin.
Translated title: Volumetric T-S analysis of water masses of Antarctic origin in the Indian sector of the Southern Ocean.
Author(s): Bozhkov, A. T.
Dmitrieva, A. A.
Menʹshenin, A. V.
Date: 1985.
Language: Russian.
In: Problemy Arktiki i Antarktiki. (1985.), Vol. 60 (1985)
Abstract: Analysis carried out in region 70-35° S and over 5° zones. From coast of Antarctica to 35° S total volume of waters of Antarctic origin amounts to 71%. Circumpolar (36.4%) and bottom (13.8%) waters, as well as surface sub-Antarctic (11.7%) and intermediate (8.8%) waters, were found to be most stable. Coastal shelf (0.2%) and surface Antarctic (0.4%) waters play important role in formation of bottom and intermediate waters circulating far from region of their formation in north to 45-35° S. Translation in Problems of the Arctic and the Antarctic, 1989, Vol.60, p.19-30.
Notes:

Problemy Arktiki i Antarktiki. Vol. 60 :17-25 (1985).

Keywords: 551.465 -- Oceanography, dynamics.
(*80) -- Southern Ocean.
(*84) -- South Indian Ocean.
SPRI record no.: 78015

MARCXML

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100 1# ‡6880-01‡aBozhkov, A. T.
242 10 ‡aVolumetric T-S analysis of water masses of Antarctic origin in the Indian sector of the Southern Ocean.‡yeng
245 10 ‡6880-02‡aObʺemnyĭ T, S-analiz vodnykh mass antarkticheskogo proiskhozhdenii︠a︡ v indiĭskom sektore I︠U︡zhnogo okeana /‡cA.T. Bozhkov, A.A. Dmitrieva, A.V. Menʹshenin.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1985.
300 ## ‡ap. 17-25 :‡bdiag., table.
500 ## ‡aProblemy Arktiki i Antarktiki. Vol. 60 :17-25 (1985).
520 3# ‡aAnalysis carried out in region 70-35° S and over 5° zones. From coast of Antarctica to 35° S total volume of waters of Antarctic origin amounts to 71%. Circumpolar (36.4%) and bottom (13.8%) waters, as well as surface sub-Antarctic (11.7%) and intermediate (8.8%) waters, were found to be most stable. Coastal shelf (0.2%) and surface Antarctic (0.4%) waters play important role in formation of bottom and intermediate waters circulating far from region of their formation in north to 45-35° S. Translation in Problems of the Arctic and the Antarctic, 1989, Vol.60, p.19-30.
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 ‡a551.465 -- Oceanography, dynamics.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*84) -- South Indian Ocean.‡2udc
700 1# ‡6880-03‡aDmitrieva, A. A.
700 1# ‡6880-04‡aMenʹshenin, A. V.
773 0# ‡6880-05‡7nnas ‡tProblemy Arktiki i Antarktiki. ‡gVol. 60 (1985) ‡wSPRI-14780
880 1# ‡6100-01/(N‡aБожков, А. Т.
880 10 ‡6245-02/(N‡aОбъемный T, С-анализ водных масс антарктического происхождения в индийском секторе Южного океана /‡cА.Т. Божков, А.А. Дмитриева, А.В. Меньшенин.
880 1# ‡6700-03/(N‡aДмитриева, А. А.
880 1# ‡6700-04/(N‡aМеньшенин, А. В.
880 0# ‡6773-05/(N‡7nnas ‡tПроблемы Арктики и Антарктики. ‡gVol. 60 (1985) ‡wSPRI-14780
917 ## ‡aUnenhanced record from Muscat, imported 2019
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