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Record #96677:

О причинах понижения концентрации атмосферного CО₂ в период максимума последнего оледенения

Title: О причинах понижения концентрации атмосферного CО₂ в период максимума последнего оледенения
Title, transliterated: O prichinakh ponizhenii︠a︡ kont︠s︡entrat︠s︡ii atmosfernogo CO₂ v period maksimuma poslednego oledenenii︠a︡ / V.A. Ri︠a︡bchenko.
Translated title: On the causes of a reduction in the concentration of atmospheric CO₂ during the maximum of the last glaciation.
Author(s): Ri︠a︡bchenko, V. A.
Date: 1989.
Language: Russian.
In: Okeanologii︠a︡. (1989.), Vol. 29(1) (1989)
Abstract: Based on combined model for seasonal evolution of carbon and thermodynamic cycles in ocean - atmosphere - land - sea-ice system of Northern Hemisphere. About 50% of reduction shown to be due to increased land-surface albedo associated with formation of ice cover. Balance explained by increased concentration of inorganic carbon, total alkalinity and primary production of phytoplankton in ocean due to erosion of organic matter from shelf.
Notes:

Okeanologii︠a︡. Vol. 29(1) :71-78 (1989).

English summary, p.78.

Keywords: 551.336 -- Ice ages.
551.464 -- Sea water, chemical properties.
551.79 -- Quaternary.
E7 -- Glaciology: glacial geology and ice ages.
(*3) -- Arctic regions.
SPRI record no.: 96677

MARCXML

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100 1# ‡6880-01‡aRi︠a︡bchenko, V. A.
242 10 ‡aOn the causes of a reduction in the concentration of atmospheric CO₂ during the maximum of the last glaciation.‡yeng
245 10 ‡6880-02‡aO prichinakh ponizhenii︠a︡ kont︠s︡entrat︠s︡ii atmosfernogo CO₂ v period maksimuma poslednego oledenenii︠a︡ /‡cV.A. Ri︠a︡bchenko.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1989.
300 ## ‡ap. 71-78 :‡btables.
500 ## ‡aOkeanologii︠a︡. Vol. 29(1) :71-78 (1989).
500 ## ‡aEnglish summary, p.78.
520 3# ‡aBased on combined model for seasonal evolution of carbon and thermodynamic cycles in ocean - atmosphere - land - sea-ice system of Northern Hemisphere. About 50% of reduction shown to be due to increased land-surface albedo associated with formation of ice cover. Balance explained by increased concentration of inorganic carbon, total alkalinity and primary production of phytoplankton in ocean due to erosion of organic matter from shelf.
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 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.464 -- Sea water, chemical properties.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
773 0# ‡6880-03‡7nnas ‡tOkeanologii︠a︡. ‡gVol. 29(1) (1989) ‡wSPRI-37085
880 1# ‡6100-01/(N‡aРябченко, В. А.
880 10 ‡6245-02/(N‡aО причинах понижения концентрации атмосферного CО₂ в период максимума последнего оледенения /‡cВ.А. Рябченко.
880 0# ‡6773-03/(N‡7nnas ‡tОкеанология. ‡gVol. 29(1) (1989) ‡wSPRI-37085
917 ## ‡aUnenhanced record from Muscat, imported 2019
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