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RUPTURE SOUDAINE EFFONDREMENT [1 record]

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Record 1 2007-10-31

English

Subject field(s)
  • Meteorological Forecasting, Data Measurement and Analysis
  • Atmospheric, Climatic and Meteorological Phenomena
CONT

At 64%, sudden collapses are most common fracture character for weak layers that produced whumpfs (fracture propagation in a weak layer, usually on low angle terrain).

CONT

About 15 years ago, some staff at Canadian parks started classifying fractures as "pops" (sudden planar fractures), and "drops" (sudden collapses) due to collapse of a thick weak layer. A recent analysis showed that pops and drops were common near human-triggered avalanches, but other types of fractures were infrequent near such avalanches.

CONT

Field tests at and above treeline continue to produce drops on a midpack facet layer and near the base of the snowpack. [Example approved by the Avalanche Bulletin Terminology Standardization Committee.]

OBS

Sudden Collapse (drop) SC: Fracture crosses the column with a single loading step and is associated with a noticeable collapse of the weak layer. [Reference: Table on Fracture Character in Small-Column Snowpack Tests.]

OBS

Prof. Bruce Jamieson of the University of Calgary has come up with a code for identifying weak layers[: Fracture Character in Small-Column Snowpack Tests. Three major classes of fractures are identified: Sudden fractures (e.g.: pops and drops), Resistant fractures (e.g.: progressive compressions and resistant planars) and Breaks (e.g.: non-planar breaks).]

OBS

drop; sudden collapse: terms officially approved by the Avalanche Bulletin Terminology Standardization Committee.

French

Domaine(s)
  • Prévisions météorologiques et mesure et analyse des données
  • Phénomènes météorologiques, climatiques et atmosphériques
CONT

Les tests sur le terrain à la ligne forestière et au-dessus de celle-ci, produisent encore des affaissements soudains sur une couche intermédiaire de faces planes et près de la base du manteau neigeux. [Exemple entériné par le Comité d'uniformisation de la terminologie des bulletins d'avalanche.]

OBS

Rupture soudaine par effondrement (affaissement soudain) SC : La rupture se produit en une seule étape de surcharge sur toute la largeur de la colonne et elle s'accompagne d'un affaissement marqué de la couche fragile. [Référence : tableau sur les Caractéristiques de la rupture lors des tests de stabilité du manteau neigeux sur petite colonne.]

OBS

affaissement soudain; rupture soudaine par effondrement : termes uniformisés par le Comité d'uniformisation de la terminologie des bulletins d'avalanche.

Spanish

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