Avalanche.report

Monday 24.08.2020

Published 24 08 2020, 10:29

Regions
Latemar, Southern Adamello, Primiero - Pale di S. Martino, Adamello - Presanella, Prealps, Northern Brenta - Peller, Cembra Valley, Bondone and Stivo, Vallarsa, Western Nonsberg Alps, Folgaria - Laverone, Southern Brenta, Fassa Valley, Sole, Pejo and Rabbi, Southern Lagorai, Ledro Valley, Northern Lagorai, Maddalene, Paganella, Marzola - Valsugana, Pine' - Mocheni Valley

AM

Danger level
Danger Level 3 - Considerabletreeline
Danger Level 2 - Moderatetreeline
Avalanche Problem
Wind-drifted snow above the treeline, N-NE-E-W-NW
Wet snow below 2400m, E-SE-S-SW-W

PM

Danger level
Danger Level 3 - Considerabletreeline
Danger Level 2 - Moderatetreeline
Avalanche Problem
Wind-drifted snow above the treeline, N-NE-E-W-NW
Wet snow below 2400m, E-SE-S-SW-W

Since the early morning the wind has been strong adjacent to ridgelines over a wide area. The sometimes strong wind will transport the old snow. As the day progresses the previously small wind slabs will increase in size once again. As a consequence of a gathering storm force wind from northwesterly directions, large surface-area wind slabs will form since Monday especially adjacent to ridgelines as well as above the tree line. The avalanche prone locations are to be found in particular on wind-loaded slopes of all aspects above approximately 2200 m and at transitions from a shallow to a deep snowpack. The fresh wind slabs are to be found in particular adjacent to ridgelines and in gullies and bowls. Over a wide area avalanche prone wind slabs will form. The sometimes large wind slabs can be released easily, even by a single winter sport participant, especially on east to south to southwest facing aspects above the tree line. This applies in particular at their margins.

Since the early morning the wind has been strong adjacent to ridgelines over a wide area. The sometimes strong wind will transport the old snow. As the day progresses the previously small wind slabs will increase in size once again. As a consequence of a gathering storm force wind from northwesterly directions, large surface-area wind slabs will form since Monday especially adjacent to ridgelines as well as above the tree line. The avalanche prone locations are to be found in particular on wind-loaded slopes of all aspects above approximately 2200 m and at transitions from a shallow to a deep snowpack. The fresh wind slabs are to be found in particular adjacent to ridgelines and in gullies and bowls. Over a wide area avalanche prone wind slabs will form. The sometimes large wind slabs can be released easily, even by a single winter sport participant, especially on east to south to southwest facing aspects above the tree line. This applies in particular at their margins.

Snowpack

dp 4: cold following warm / warm following cold
dp 7: snow-poor zones in snow-rich surrounding

Since the early morning the wind has been strong adjacent to ridgelines over a wide area. The sometimes strong wind will transport the old snow. As the day progresses the previously small wind slabs will increase in size once again. As a consequence of a gathering storm force wind from northwesterly directions, large surface-area wind slabs will form since Monday especially adjacent to ridgelines as well as above the tree line. The avalanche prone locations are to be found in particular on wind-loaded slopes of all aspects above approximately 2200 m and at transitions from a shallow to a deep snowpack. The fresh wind slabs are to be found in particular adjacent to ridgelines and in gullies and bowls. Over a wide area avalanche prone wind slabs will form. The sometimes large wind slabs can be released easily, even by a single winter sport participant, especially on east to south to southwest facing aspects above the tree line. This applies in particular at their margins.

Tendency

Since the early morning the wind has been strong adjacent to ridgelines over a wide area. The sometimes strong wind will transport the old snow. As the day progresses the previously small wind slabs will increase in size once again. As a consequence of a gathering storm force wind from northwesterly directions, large surface-area wind slabs will form since Monday especially adjacent to ridgelines as well as above the tree line. The avalanche prone locations are to be found in particular on wind-loaded slopes of all aspects above approximately 2200 m and at transitions from a shallow to a deep snowpack. The fresh wind slabs are to be found in particular adjacent to ridgelines and in gullies and bowls. Over a wide area avalanche prone wind slabs will form. The sometimes large wind slabs can be released easily, even by a single winter sport participant, especially on east to south to southwest facing aspects above the tree line. This applies in particular at their margins.