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Record #88391:
- #88391
Main publication details
MARC recordTwo types of intraglacial meltwater regime for the Bertil Glacier, Svalbard / V.V. Gokhman.
| Title: | Two types of intraglacial meltwater regime for the Bertil Glacier, Svalbard / V.V. Gokhman. |
| Author(s): | Gokhman, V. V. |
| Date: | 1987. |
| 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: | Polar Geography and Geology. (1987.), Vol. 11(4) (1987) |
| Abstract: | In 1960s and 1970s, runoff was faster than in 1980s. Volume of this englacial runoff made up of 40% of total runoff, compared with 10-20% for slower type. Suggests cause of these two types, possibly connected with progressive freezing of glacier and changes in hydrothermal regime. |
| Notes: | Polar Geography and Geology. Vol. 11(4) :241-248 (1987). Translated from Materialy Glyatsiologicheskikh Issledovaniy, 1987, No.59, p.152-156. |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.86 -- Glacier streams. 556 -- Hydrology. E11 -- Glaciology: glaciohydrology. (*32) -- Svalbard. (*324) -- Spitsbergen. |
| SPRI record no.: | 88391 |
LDR 01708naa#a2200000#a#4500 001 SPRI-88391 005 20230328153908.0 007 ta 008 230328s1987####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-88391 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGokhman, V. V. 240 10 ‡6880-01‡aO dvukh tipakh rezhima vnutrilednikovykh vod lednika Bertilʹ na Shpit︠s︡bergene.‡lRussian 245 10 ‡aTwo types of intraglacial meltwater regime for the Bertil Glacier, Svalbard /‡cV.V. Gokhman. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 241-248 :‡bdiag., table. 500 ## ‡aPolar Geography and Geology. Vol. 11(4) :241-248 (1987). 500 ## ‡aTranslated from Materialy Glyatsiologicheskikh Issledovaniy, 1987, No.59, p.152-156. 520 3# ‡aIn 1960s and 1970s, runoff was faster than in 1980s. Volume of this englacial runoff made up of 40% of total runoff, compared with 10-20% for slower type. Suggests cause of these two types, possibly connected with progressive freezing of glacier and changes in hydrothermal regime. 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 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.86 -- Glacier streams.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 651 #7 ‡a(*32) -- Svalbard.‡2udc 651 #7 ‡a(*324) -- Spitsbergen.‡2udc 773 0# ‡7nnas ‡tPolar Geography and Geology. ‡gVol. 11(4) (1987) ‡wSPRI-56066 880 10 ‡6240-01/(N‡aО двух типах режима внутриледниковых вод ледника Бертиль на Шпицбергене.‡lRussian 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230328