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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #111186:

Experimental and theoretical study of the dynamics of powder snow avalanches / Pierre Beghin, Xavier Olagne.

Title: Experimental and theoretical study of the dynamics of powder snow avalanches / Pierre Beghin, Xavier Olagne.
Author(s): Beghin, Pierre.
Olagne, Xavier.
Date: 1991.
In: Cold Regions Science and Technology. (1991.), Vol. 19(3) (1991)
Abstract: Experimental results in water tank show that "thermal theory" is applicable to 3-D flow of buoyant cloud for slope angles between 10 and 90°. Spatial growth rates in height and length are linear functions of shape angle, whereas growth has nearly constant value. Results can be extrapolated to powder snow avalanche to calculate flow variables along track.
Notes:

Cold Regions Science and Technology. Vol. 19(3) :317-326 (1991).

Keywords: 551.578.481 -- Avalanches, types.
551.578.482 -- Avalanches. Theory, causes.
E10 -- Glaciology: snow and avalanches.
SPRI record no.: 111186

MARCXML

LDR 01163naa#a2200000#a#4500
001 SPRI-111186
005 20240419123835.0
007 ta
008 240419s1991####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-111186
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aBeghin, Pierre.
245 10 ‡aExperimental and theoretical study of the dynamics of powder snow avalanches /‡cPierre Beghin, Xavier Olagne.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 317-326 :‡bill., diags.
500 ## ‡aCold Regions Science and Technology. Vol. 19(3) :317-326 (1991).
520 3# ‡aExperimental results in water tank show that "thermal theory" is applicable to 3-D flow of buoyant cloud for slope angles between 10 and 90°. Spatial growth rates in height and length are linear functions of shape angle, whereas growth has nearly constant value. Results can be extrapolated to powder snow avalanche to calculate flow variables along track.
650 07 ‡a551.578.481 -- Avalanches, types.‡2udc
650 07 ‡a551.578.482 -- Avalanches. Theory, causes.‡2udc
650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local
700 1# ‡aOlagne, Xavier.
773 0# ‡7nnas ‡tCold Regions Science and Technology. ‡gVol. 19(3) (1991) ‡wSPRI-59075
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419