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Record #166749:

Thickness of ice-bonded permafrost in the eastern part of the Laptev Sea shelf (Results of modelling) / N.N. Romanovskii, A.L. Kholodov, A.V. Gavrilov, V.E. Tumskoy, H.-W. Hubberten, H. Kassens.

Title: Thickness of ice-bonded permafrost in the eastern part of the Laptev Sea shelf (Results of modelling) / N.N. Romanovskii, A.L. Kholodov, A.V. Gavrilov, V.E. Tumskoy, H.-W. Hubberten, H. Kassens.
Author(s): Romanovskii, N. N.
Kholodov, A. L.
Gavrilov, A. V.
Tumskoy, V. E.
Hubberten, H. -W.
Kassens, H.
Date: 2003.
Language: Russian 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.
In: Earth's Cryosphere. (2003.), Special issue (2003)
Abstract: Investigates thickness of offshore permafrost on eastern Laptev Sea shelf and compiles schematic map of its distribution. Presents computer modelling based on specified paleogeographical scenario and geological model for last glacioeustatic cycle. Uses new computational scheme and refined data to derive more precise distribution of permafrost in eastern part. Calculated thickness of ice-bonded permafrost increases northwards for given sea depth and decreases with increasing sea depth, reaching maximum of 450-520 m. Describes ongoing permafrost degradation due to geothermal heat flow since last 18 kyr BP. Concludes layer of cryotic deposits 70 to 120 m thick underlies permafrost.
Notes:

Earth's Cryosphere. Special issue :65-75 (2003).

Translated from Kriosfera Zemli, 1999 3(2) :22-32.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.341 -- Permafrost and frozen ground, equipment for investigating.
551.345 -- Permafrost. Cryopedology.
551.345.1 -- Permafrost, surveys.
551.345.2 -- Permafrost, formation and decay.
551.462.32 -- Continental shelves.
519.673 -- Modelling.
551.8 -- Palaeogeography: Holocene.
084.3 -- Atlases, charts and maps.
551.461.2 -- Sea level, fluctuations.
551.465.77 -- Oceans, heat flux across floor.
E8 -- Glaciology: frost action and permafrost.
(*60) -- Arctic Ocean and adjacent waters.
(*68) -- Arctic Ocean, seas adjacent to Russia.
(*684) -- Laptev Sea.
SPRI record no.: 166749

MARCXML

LDR 02823naa#a2200000#a#4500
001 SPRI-166749
005 20220927112241.0
007 ta
008 220927s2003####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-166749
040 ## ‡aUkCU-P‡beng‡eaacr
240 10 ‡6880-01‡aMoshchnostʹ merzlykh tolshch vostochnoĭ chasti shelʹfa mori︠a︡ Laptevykh.‡lRussian
245 00 ‡aThickness of ice-bonded permafrost in the eastern part of the Laptev Sea shelf (Results of modelling) /‡cN.N. Romanovskii, A.L. Kholodov, A.V. Gavrilov, V.E. Tumskoy, H.-W. Hubberten, H. Kassens.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 65-75 :‡bdiags., tables, maps.
500 ## ‡aEarth's Cryosphere. Special issue :65-75 (2003).
500 ## ‡aTranslated from Kriosfera Zemli, 1999 3(2) :22-32.
520 3# ‡aInvestigates thickness of offshore permafrost on eastern Laptev Sea shelf and compiles schematic map of its distribution. Presents computer modelling based on specified paleogeographical scenario and geological model for last glacioeustatic cycle. Uses new computational scheme and refined data to derive more precise distribution of permafrost in eastern part. Calculated thickness of ice-bonded permafrost increases northwards for given sea depth and decreases with increasing sea depth, reaching maximum of 450-520 m. Describes ongoing permafrost degradation due to geothermal heat flow since last 18 kyr BP. Concludes layer of cryotic deposits 70 to 120 m thick underlies permafrost.
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 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.341 -- Permafrost and frozen ground, equipment for investigating.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a551.345.1 -- Permafrost, surveys.‡2udc
650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc
650 07 ‡a551.462.32 -- Continental shelves.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.8 -- Palaeogeography: Holocene.‡2udc
650 07 ‡a084.3 -- Atlases, charts and maps.‡2udc
650 07 ‡a551.461.2 -- Sea level, fluctuations.‡2udc
650 07 ‡a551.465.77 -- Oceans, heat flux across floor.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*68) -- Arctic Ocean, seas adjacent to Russia.‡2udc
651 #7 ‡a(*684) -- Laptev Sea.‡2udc
700 1# ‡aRomanovskii, N. N.
700 1# ‡aKholodov, A. L.
700 1# ‡aGavrilov, A. V.
700 1# ‡aTumskoy, V. E.
700 1# ‡aHubberten, H. -W.
700 1# ‡aKassens, H.
773 0# ‡7nnas ‡tEarth's Cryosphere. ‡gSpecial issue (2003) ‡wSPRI-166654
880 10 ‡6240-01/(N‡aМощность мерзлых толщ восточной части шельфа моря Лаптевых.‡lRussian
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220927