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Record #181195:

Влияние глобального потепления оптимум голоцена на состояние оледенения в арктических и субарктических районах России

Title: Влияние глобального потепления оптимум голоцена на состояние оледенения в арктических и субарктических районах России
Title, transliterated: Vlii︠a︡nie globalʹnogo poteplenii︠a︡ optimum golot︠s︡ena na sostoi︠a︡nie oledenenii︠a︡ v arkticheskikh i subarkticheskikh raĭonakh Rossii / N.V. Davidovich.
Translated title: Effect of global warming in the Holocene optimum on the glaciation state in the Arctic and sub-Arctic regions of Russia.
Author(s): Davidovich, N. V.
Date: 2006.
Language: Russian.
In: Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (2006.), Vol. 100 (2006)
Abstract: Presents methodology and results of reconstruction of major glaciological features at high latitudes during Holocene climatic optimum, using examples of contemporary glaciated regions of Novaya Zemlya, Byrranga Range and Orulgan Range. Palaeglaciologic calculations show that ubiquitous rise of equilibrium line altitude (ELA) caused cardinal changes in glaciation. ELA at Northern island of Novaya Zemlya was higher than contemporary one and higher even than both surface of contemporary ice sheet and absolute altitude of bedrock. Estimation of ice mass decrease confirm high probability of disappearance of ice sheet during climatic optimum. This could also have occurred in low-mountainous areas of Byrranga range and northern part of Orulgan range. Discusses possibilities of continuous glacier existence in areas whose highest altitudes exceeded ELA and where increase of solid precipitation and mass exchange promoted more stable existence than at present.
Notes:

Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 100 :114-127 (2006).

English summary and figure captions.

Keywords: 551.32 -- Glaciology.
551.321 -- Glaciological methods and instruments.
551.58 -- Climatology.
551.8 -- Palaeogeography.
551.794 -- Holocene.
551.324 -- Land ice.
551.324.43 -- Land ice, regime and mass balance.
551.324.435 -- Firn line.
551.588.5 -- Climate, relationship with ice.
551.324.22 -- Glaciers.
551.324.63 -- Land ice, advance and retreat.
551.324.431 -- Land ice, accumulation.
E5 -- Glaciology: land ice.
(*526) -- Novaya Zemlya.
(*531.41) -- Taymyrskiy Avtonomnyy Okrug.
(*531.3) -- Yakutiya. Respublika Sakha.
SPRI record no.: 181195

MARCXML

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001 SPRI-181195
005 20240328132151.0
007 ta
008 240328s2006####xx#a##|##|###|0||#0|rus#d
035 ## ‡aSPRI-181195
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aDavidovich, N. V.
242 10 ‡aEffect of global warming in the Holocene optimum on the glaciation state in the Arctic and sub-Arctic regions of Russia.‡yeng
245 10 ‡6880-02‡aVlii︠a︡nie globalʹnogo poteplenii︠a︡ optimum golot︠s︡ena na sostoi︠a︡nie oledenenii︠a︡ v arkticheskikh i subarkticheskikh raĭonakh Rossii /‡cN.V. Davidovich.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2006.
300 ## ‡ap. 114-127 :‡bill., diags., tables.
500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 100 :114-127 (2006).
500 ## ‡aEnglish summary and figure captions.
520 3# ‡aPresents methodology and results of reconstruction of major glaciological features at high latitudes during Holocene climatic optimum, using examples of contemporary glaciated regions of Novaya Zemlya, Byrranga Range and Orulgan Range. Palaeglaciologic calculations show that ubiquitous rise of equilibrium line altitude (ELA) caused cardinal changes in glaciation. ELA at Northern island of Novaya Zemlya was higher than contemporary one and higher even than both surface of contemporary ice sheet and absolute altitude of bedrock. Estimation of ice mass decrease confirm high probability of disappearance of ice sheet during climatic optimum. This could also have occurred in low-mountainous areas of Byrranga range and northern part of Orulgan range. Discusses possibilities of continuous glacier existence in areas whose highest altitudes exceeded ELA and where increase of solid precipitation and mass exchange promoted more stable existence than at present.
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 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.8 -- Palaeogeography.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc
650 07 ‡a551.324.435 -- Firn line.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.324.431 -- Land ice, accumulation.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*526) -- Novaya Zemlya.‡2udc
651 #7 ‡a(*531.41) -- Taymyrskiy Avtonomnyy Okrug.‡2udc
651 #7 ‡a(*531.3) -- Yakutiya. Respublika Sakha.‡2udc
773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 100 (2006) ‡wSPRI-33585
880 1# ‡6100-01/(N‡aДавидович, Н. В.
880 10 ‡6245-02/(N‡aВлияние глобального потепления оптимум голоцена на состояние оледенения в арктических и субарктических районах России /‡cН.В. Давидович.
880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 100 (2006) ‡wSPRI-33585
916 ## ‡a2007/12/07 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328 ‡bRF