Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #179919:
- #179919
Main publication details
MARC recordСравнительный анализ палеоклиматических условий Прибайкалья и Камчатки на основе моделей оледенения последнего ледникового максимума
| Title: | Сравнительный анализ палеоклиматических условий Прибайкалья и Камчатки на основе моделей оледенения последнего ледникового максимума |
| Title, transliterated: | Sravnitelʹnyĭ analiz paleoklimaticheskikh usloviĭ Pribaĭkalʹi︠a︡ i Kamchatki na osnove modeleĭ oledenenii︠a︡ poslednego lednikovogo maksimuma / Ė.I︠U︡. Osipov, O.S. Savoskul. |
| Translated title: | Comparative analysis of palaeoenvironment in Baikal area and Kamchatka based on the models of the Last Glacial Maximum. |
| Author(s): | Osipov, Ė. I︠U︡. Savoskul, O. S. |
| Date: | 2006. |
| Language: | Russian. |
| In: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (2006.), Vol. 101 (2006) |
| Abstract: | Infers palaeoglaciological models for Last Glacial Maximum (LGM, 18-20 ky) using geomorphological data from Barguzinsky Ridge (Lake Baikal region) and Sredinny Ridge (Kamchatka). Analyses models to estimate equilibrium line altitudes of representative palaeoglaciers, obtaining ELA depressions of 1000-1100 m for Barguzinsky Ridge and 700-800 m for Sredinny Ridge. Uses empirical glacio-climate model to estimate LGM palaeoclimate parameters. Moisture estimates based on palynological data and global reconstructions suggest that LGM precipitation was approximately 1.5-2 times lower than today in Baikal and 1.2-1.5 times lower in Kamchatka. Suggests reconstructed palaeoglaciers owed their existence to summer air temperatures 7-9°C lower in Baikal and 5-7°C lower in Kamchatka. |
| Notes: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 101 :77-82 (2006). English summary and captions. |
| Keywords: | 551.32 -- Glaciology. 551.33 -- Glacial geology. 551.324 -- Land ice. 551.336 -- Ice ages. 551.58 -- Climatology. 551.583.3 -- Climatic changes, Quaternary. 551.4 -- Geomorphology. 551.324.22 -- Glaciers. 551.324.61 -- Land ice, cycle of growth and decay. 551.324.435 -- Firn line. 550.93 -- Geochronology. 581.081.3 -- Pollen analysis. 551.324.431 -- Land ice, accumulation. 551.524 -- Air temperature. 519.673 -- Modelling. E9 -- Glaciology: meteorology and climatology. (*532.5) -- Irkutskaya Oblast'. (*532.6) -- Respublika Buryatiya. (*531.25) -- Kamchatskaya Oblast'. |
| SPRI record no.: | 179919 |
LDR 03247naa#a2200000#a#4500 001 SPRI-179919 005 20230331014823.0 007 ta 008 230331s2006####xx#ab#|##|###|0||#0|rus#d 035 ## ‡aSPRI-179919 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aOsipov, Ė. I︠U︡. 242 10 ‡aComparative analysis of palaeoenvironment in Baikal area and Kamchatka based on the models of the Last Glacial Maximum.‡yeng 245 10 ‡6880-02‡aSravnitelʹnyĭ analiz paleoklimaticheskikh usloviĭ Pribaĭkalʹi︠a︡ i Kamchatki na osnove modeleĭ oledenenii︠a︡ poslednego lednikovogo maksimuma /‡cĖ.I︠U︡. Osipov, O.S. Savoskul. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2006. 300 ## ‡ap. 77-82 :‡bill., diag., map. 500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 101 :77-82 (2006). 500 ## ‡aEnglish summary and captions. 520 3# ‡aInfers palaeoglaciological models for Last Glacial Maximum (LGM, 18-20 ky) using geomorphological data from Barguzinsky Ridge (Lake Baikal region) and Sredinny Ridge (Kamchatka). Analyses models to estimate equilibrium line altitudes of representative palaeoglaciers, obtaining ELA depressions of 1000-1100 m for Barguzinsky Ridge and 700-800 m for Sredinny Ridge. Uses empirical glacio-climate model to estimate LGM palaeoclimate parameters. Moisture estimates based on palynological data and global reconstructions suggest that LGM precipitation was approximately 1.5-2 times lower than today in Baikal and 1.2-1.5 times lower in Kamchatka. Suggests reconstructed palaeoglaciers owed their existence to summer air temperatures 7-9°C lower in Baikal and 5-7°C lower in Kamchatka. 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 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.61 -- Land ice, cycle of growth and decay.‡2udc 650 07 ‡a551.324.435 -- Firn line.‡2udc 650 07 ‡a550.93 -- Geochronology.‡2udc 650 07 ‡a581.081.3 -- Pollen analysis.‡2udc 650 07 ‡a551.324.431 -- Land ice, accumulation.‡2udc 650 07 ‡a551.524 -- Air temperature.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(*532.5) -- Irkutskaya Oblast'.‡2udc 651 #7 ‡a(*532.6) -- Respublika Buryatiya.‡2udc 651 #7 ‡a(*531.25) -- Kamchatskaya Oblast'.‡2udc 700 1# ‡6880-03‡aSavoskul, O. S. 773 0# ‡6880-04‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 101 (2006) ‡wSPRI-33585 880 1# ‡6100-01/(N‡aОсипов, Э. Ю. 880 10 ‡6245-02/(N‡aСравнительный анализ палеоклиматических условий Прибайкалья и Камчатки на основе моделей оледенения последнего ледникового максимума /‡cЭ.Ю. Осипов, О.С. Савоскул. 880 1# ‡6700-03/(N‡aСавоскул, О. С. 880 0# ‡6773-04/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 101 (2006) ‡wSPRI-33585 916 ## ‡a2007/07/23 -- RF 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230331 ‡bRF