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Record #144350:
Active layer thermal regime at three rock glaciers in Greenland / Ole Humlum.
Title: | Active layer thermal regime at three rock glaciers in Greenland / Ole Humlum. |
Author(s): | Humlum, Ole. |
Date: | 1997. |
In: | Permafrost and Periglacial Processes. (1997.), Vol. 8(4) (1997) |
Abstract: | Two glaciers are talus-derived and one is glacier-derived. Thermal characteristics of very coarse grained active layer are described and compared with those of other types of active layer. Conductive and non-conductive heat transfer seem to be important on both types. In general, coarse surface seems to act as thermal filter, which may explain why rock glaciers tend to be more frequent in dry continental areas. |
Notes: | Permafrost and Periglacial Processes. Vol. 8(4) :383-408 (1997). |
Keywords: | 536.2 -- Heat, transmission. 551.343.4 -- Rock glaciers. A -- Geophysical sciences (general). (*3) -- Arctic regions. (*38) -- Greenland. |
SPRI record no.: | 144350 |
LDR 01212naa#a2200000#a#4500 001 SPRI-144350 005 20230528130642.0 007 ta 008 230528s1997####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-144350 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHumlum, Ole. 245 10 ‡aActive layer thermal regime at three rock glaciers in Greenland /‡cOle Humlum. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1997. 300 ## ‡ap. 383-408 :‡bill., diags. 500 ## ‡aPermafrost and Periglacial Processes. Vol. 8(4) :383-408 (1997). 520 3# ‡aTwo glaciers are talus-derived and one is glacier-derived. Thermal characteristics of very coarse grained active layer are described and compared with those of other types of active layer. Conductive and non-conductive heat transfer seem to be important on both types. In general, coarse surface seems to act as thermal filter, which may explain why rock glaciers tend to be more frequent in dry continental areas. 650 07 ‡a536.2 -- Heat, transmission.‡2udc 650 07 ‡a551.343.4 -- Rock glaciers.‡2udc 650 07 ‡aA -- Geophysical sciences (general).‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 773 0# ‡7nnas ‡tPermafrost and Periglacial Processes. ‡gVol. 8(4) (1997) ‡wSPRI-102743 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230528