skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View 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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #119593:

Induced flow channels in a natural snowpack / M.R. Albert, W.R. McGilvary, H.J. Greenan.

Title: Induced flow channels in a natural snowpack / M.R. Albert, W.R. McGilvary, H.J. Greenan.
Author(s): Albert, M. R.
McGilvary, W. R.
Greenan, H. J.
Date: 1992.
In: Eastern Snow Conference. Proceedings. (1992.), Vol. 49th Annual Meeting (1992)
Abstract: By examining response of two adjacent identical lysimeters. one with disturbed snow cover and one without, number of vertical flow paths for shallow layered snowpacks appears to have large influence on snowmelt discharge. For ripe homogeneous snowpacks with large discharge rates, induced vertical flow paths have little effect on discharge. Layering effects influence discharge through significant portion of snowmelt season.
Notes:

Eastern Snow Conference. Proceedings. Vol. 49th Annual Meeting :55-60 (1992).

Keywords: 551.578.46 -- Snow cover and snow patches.
551.578.462 -- Snow cover, ablation.
551.579.2 -- Water supply from snow.
556 -- Hydrology.
E11 -- Glaciology: glaciohydrology.
SPRI record no.: 119593

MARCXML

LDR 01338naa#a2200000#a#4500
001 SPRI-119593
005 20221002044415.0
007 ta
008 221002s1992####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-119593
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aAlbert, M. R.
245 10 ‡aInduced flow channels in a natural snowpack /‡cM.R. Albert, W.R. McGilvary, H.J. Greenan.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 55-60 :‡bdiags.
500 ## ‡aEastern Snow Conference. Proceedings. Vol. 49th Annual Meeting :55-60 (1992).
520 3# ‡aBy examining response of two adjacent identical lysimeters. one with disturbed snow cover and one without, number of vertical flow paths for shallow layered snowpacks appears to have large influence on snowmelt discharge. For ripe homogeneous snowpacks with large discharge rates, induced vertical flow paths have little effect on discharge. Layering effects influence discharge through significant portion of snowmelt season.
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.578.462 -- Snow cover, ablation.‡2udc
650 07 ‡a551.579.2 -- Water supply from snow.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local
700 1# ‡aMcGilvary, W. R.
700 1# ‡aGreenan, H. J.
773 0# ‡7nnas ‡tEastern Snow Conference. Proceedings. ‡gVol. 49th Annual Meeting (1992) ‡wSPRI-23848
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221002