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Record #148542:
Formation of ice layers by infiltration and refreezing of meltwater / W.T. Pfeffer, N.F. Humphrey.
Title: | Formation of ice layers by infiltration and refreezing of meltwater / W.T. Pfeffer, N.F. Humphrey. |
Author(s): | Pfeffer, W. T. Humphrey, N. F. |
Date: | 1998. |
In: | Annals of Glaciology. (1998.), Vol. 26 (1998) |
Abstract: | Studies process of ice-layer formation by modelling competition between infiltration of water across stratigraphic boundary in layered porous media and loss of water by refreezing. Contributes to discussion of how ice layers originate. Indicates increased frequency of ice layers in snow derives from greater temperature contrast between winter and summer conditions. |
Notes: | Annals of Glaciology. Vol. 26 :83-91 (1998). Papers from the International Symposium on Snow and Avalanches, 26--30 May 1997, Chamonix Mont-Blanc, France, D.M. McClung (Editor) |
Keywords: | 551.5 -- Meteorology. 551.578.46 -- Snow cover and snow patches. 536.5 -- Temperature measurement and control. 551.578.465 -- Snow cover, stratification. 556 -- Hydrology. 551.32 -- Glaciology. 551.322 -- Ice and snow. 551.321.82 -- Snow analogues, experimental. 519.673 -- Modelling. E9 -- Glaciology: meteorology and climatology. (*384) -- West Greenland. |
SPRI record no.: | 148542 |
LDR 01620naa#a2200000#a#4500 001 SPRI-148542 005 20240329125415.0 007 ta 008 240329s1998####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-148542 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPfeffer, W. T. 245 10 ‡aFormation of ice layers by infiltration and refreezing of meltwater /‡cW.T. Pfeffer, N.F. Humphrey. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1998. 300 ## ‡ap. 83-91 :‡bdiags., tables. 500 ## ‡aAnnals of Glaciology. Vol. 26 :83-91 (1998). 500 ## ‡aPapers from the International Symposium on Snow and Avalanches, 26--30 May 1997, Chamonix Mont-Blanc, France, D.M. McClung (Editor) 520 3# ‡aStudies process of ice-layer formation by modelling competition between infiltration of water across stratigraphic boundary in layered porous media and loss of water by refreezing. Contributes to discussion of how ice layers originate. Indicates increased frequency of ice layers in snow derives from greater temperature contrast between winter and summer conditions. 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a536.5 -- Temperature measurement and control.‡2udc 650 07 ‡a551.578.465 -- Snow cover, stratification.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.322 -- Ice and snow.‡2udc 650 07 ‡a551.321.82 -- Snow analogues, experimental.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(*384) -- West Greenland.‡2udc 700 1# ‡aHumphrey, N. F. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 26 (1998) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329