link Link to website https://avalanche.report/bulletin/2022-01-15 simple_link Link to the simplified website https://avalanche.report/simple/2022-01-15/en.html fd_albina_map.jpg Danger rating map (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_albina_map.jpg fd_tyrol_map.jpg Danger rating map Tirol (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_tyrol_map.jpg fd_southtyrol_map.jpg Danger rating map Southtyrol (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_southtyrol_map.jpg fd_trentino_map.jpg Danger rating map Trentino (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_trentino_map.jpg pdf PDF https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/2022-01-15_en.pdf tyrol_pdf PDF Tirol https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/2022-01-15_AT-07_en.pdf southtyrol_pdf PDF Southtyrol https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/2022-01-15_IT-32-BZ_en.pdf trentino_pdf PDF Trentino https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/2022-01-15_IT-32-TN_en.pdf fd_overlay.png Danger rating overlay (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_overlay.png fd_regions.json GeoJSON for regions (whole day) https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/fd_regions.json dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/026eabef-335c-40eb-b46b-dea527007d35.jpg website Link to region on the website https://avalanche.report/bulletin/2022-01-15?region=026eabef-335c-40eb-b46b-dea527007d35 2022-01-14T16:00:00.023922Z 2022-01-14T23:00:00Z 2022-01-15T23:00:00Z Avalanche.report https://avalanche.report Sexten Dolomites Latemar Southern Adamello Adamello - Presanella Northern Brenta - Peller Southern Brenta Southern Lagorai Northern Lagorai Allgäu Alps Eastern Lechtal Alps - Ammergau Alps Western Lechtal Alps Central Lechtal Alps Grieskogel Mountains Val Müstair Alps Western Verwall Mountains Langtaufers Eastern Verwall Mountains Schnals Ridge Silvretta Southern Stubai Alps Samnaun Mountains Southern Zillertal Alps and High Tauern Northern Oetz and Stubai Alps Saldurn-Mastaun Ridge Western Tuxer Alps Texel Mountains Eastern Tuxer Alps Sarntal Alps Western Pfunderer Mountains Glockturm Range Maddalene Eastern Pfunderer Mountains Durreck Range Weißkugel Range Western Rieserferner Mountains Gurgler Range Western Deferegger Alps Central Stubai Alps Ortler Range Northern Zillertal Alps Ulten Valley Venediger Range Eastern Rieserferner Mountains Glockner Range Gröden Dolomites Primiero - Pale di S. Martino Eastern Deferegger Alps Prags Dolomites Schober Mountains Lienzer Dolomites Fassa Valley Sole, Pejo and Rabbi moderate 2400 no_rating no_rating low 2400 no_rating no_rating dp7 dp6 wind_drifted_snow NW W NE N E 2400 moderate moderate 2 2 2 steady 2022-01-15T23:00:00Z 2022-01-16T23:00:00Z A generally favourable avalanche situation will prevail. In isolated cases avalanches can be triggered in the faceted old snow and reach medium size. The avalanche prone locations are to be found on extremely steep shady slopes above approximately 2400 m and in gullies and bowls, and behind abrupt changes in the terrain. Caution is to be exercised in particular in areas where the snow cover is rather shallow. Older wind slabs are to be evaluated with care and prudence in extremely steep terrain. <br/> As a consequence of warming during the day and solar radiation individual wet and gliding avalanches are possible as the day progresses. This applies in particular on very steep sunny slopes. <br/> Apart from the danger of being buried, restraint should be exercised as well in view of the danger of avalanches sweeping people along and giving rise to falls. Sunshine and high temperatures will give rise to gradual consolidation of the snowpack. Somewhat older wind slabs have bonded quite well with the old snowpack. They are in individual cases still prone to triggering. Field observations and stability tests confirm good snowpack stability. <br/> In very isolated cases weak layers exist in the centre of the old snowpack especially on shady slopes. This applies in particular above approximately 2400 m. <br/> At elevated altitudes snow depths vary greatly, depending on the infuence of the wind. A generally favourable avalanche situation will prevail. Older wind slabs are to be evaluated with care and prudence especially in extremely steep terrain. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/eb93a652-b5e9-4e1d-a234-814dc9b88876.jpg website Link to region on the website https://avalanche.report/bulletin/2022-01-15?region=eb93a652-b5e9-4e1d-a234-814dc9b88876 2022-01-14T16:00:00.023922Z 2022-01-14T23:00:00Z 2022-01-15T23:00:00Z Avalanche.report https://avalanche.report Prealps Cembra Valley Bondone and Stivo Vallarsa Western Nonsberg Alps Folgaria - Laverone Ledro Valley Eastern Nonsberger Alps Paganella Northern Dolomites of Fiemme Marzola - Valsugana Pine' - Mocheni Valley low no_rating no_rating dp6 dp7 steady 2022-01-15T23:00:00Z 2022-01-16T23:00:00Z A generally favourable avalanche situation will prevail. Avalanches can be released in near-surface layers, mostly by large additional loads. Individual avalanche prone locations are to be found in particular on extremely steep shady slopes above approximately 2400 m and in gullies and bowls, and behind abrupt changes in the terrain. Caution is to be exercised in particular in areas where the snow cover is rather shallow. Older wind slabs are to be evaluated with care and prudence in extremely steep terrain. <br/> As a consequence of warming during the day and solar radiation individual wet and gliding avalanches are possible as the day progresses. Apart from the danger of being buried, restraint should be exercised as well in view of the danger of avalanches sweeping people along and giving rise to falls. Sunshine and high temperatures will give rise to gradual consolidation of the snowpack. Somewhat older wind slabs have bonded quite well with the old snowpack. They are in individual cases still prone to triggering. Field observations and stability tests confirm good snowpack stability. <br/> In very isolated cases weak layers exist in the centre of the old snowpack especially on shady slopes. This applies in particular above approximately 2400 m. <br/> At elevated altitudes snow depths vary greatly, depending on the infuence of the wind. A generally favourable avalanche situation will prevail. Older wind slabs are to be evaluated with care and prudence especially in extremely steep terrain. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2022-01-15/2022-01-14_16-00-00/3a787b22-f186-44da-89e4-edda925953f3.jpg website Link to region on the website https://avalanche.report/bulletin/2022-01-15?region=3a787b22-f186-44da-89e4-edda925953f3 2022-01-14T16:00:00Z 2022-01-14T23:00:00Z 2022-01-15T23:00:00Z Avalanche.report https://avalanche.report Karwendel Mountains Brandenberg Alps Western Kitzbühel Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Mieming Mountains low no_rating no_rating dp6 dp7 steady 2022-01-15T23:00:00Z 2022-01-16T23:00:00Z A generally favourable avalanche situation will prevail. Avalanches can be released in near-surface layers, mostly by large additional loads. Individual avalanche prone locations are to be found in particular on extremely steep shady slopes above approximately 2400 m and in gullies and bowls, and behind abrupt changes in the terrain. Caution is to be exercised in particular in areas where the snow cover is rather shallow. Older wind slabs are to be evaluated with care and prudence in extremely steep terrain. <br/> As a consequence of warming during the day and solar radiation individual wet and gliding avalanches are possible as the day progresses. Apart from the danger of being buried, restraint should be exercised as well in view of the danger of avalanches sweeping people along and giving rise to falls. Sunshine and high temperatures will give rise to gradual consolidation of the snowpack. Somewhat older wind slabs have bonded quite well with the old snowpack. They are in individual cases still prone to triggering. Field observations and stability tests confirm good snowpack stability. <br/> In very isolated cases weak layers exist in the centre of the old snowpack especially on shady slopes. This applies in particular above approximately 2400 m. <br/> At elevated altitudes snow depths vary greatly, depending on the infuence of the wind. A generally favourable avalanche situation will prevail. Older wind slabs are to be evaluated with care and prudence especially in extremely steep terrain.