link Link to website https://avalanche.report/bulletin/2021-02-14 simple_link Link to the simplified website https://avalanche.report/simple/2021-02-14/en.html fd_albina_map.jpg Danger rating map (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_albina_map.jpg fd_tyrol_map.jpg Danger rating map Tirol (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_tyrol_map.jpg fd_southtyrol_map.jpg Danger rating map Southtyrol (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_southtyrol_map.jpg fd_trentino_map.jpg Danger rating map Trentino (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_trentino_map.jpg pdf PDF https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/2021-02-14_en.pdf tyrol_pdf PDF Tirol https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/2021-02-14_AT-07_en.pdf southtyrol_pdf PDF Southtyrol https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/2021-02-14_IT-32-BZ_en.pdf trentino_pdf PDF Trentino https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/2021-02-14_IT-32-TN_en.pdf fd_overlay.png Danger rating overlay (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_overlay.png fd_regions.json GeoJSON for regions (whole day) https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/fd_regions.json dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/9e3c8bf7-2a48-4605-bddc-025aaa60f56c.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-14?region=9e3c8bf7-2a48-4605-bddc-025aaa60f56c 2021-02-13T16:00:00Z 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Avalanche.report https://avalanche.report 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 considerable treeline no_rating no_rating moderate treeline no_rating no_rating dp6 wind_drifted_snow SE SW E W NW S N NE treeline considerable considerable 3 3 2 gliding_snow SE SW W NW S 2200 moderate moderate 1 2 persistent_weak_layers SE E SW W NW S N NE treeline considerable considerable 2 2 steady 2021-02-14T23:00:00Z 2021-02-15T23:00:00Z Fresh wind slabs represent the main danger. At elevated altitudes a considerable avalanche danger will still be encountered. The new snow and wind slabs remain very prone to triggering in all aspects above the tree line. This applies in particular on very steep slopes, and adjacent to ridgelines. The fresh wind slabs can be released easily. or in isolated cases naturally, in all aspects and generally above the tree line. The number and size of avalanche prone locations will increase with altitude. <br/> Weak layers in the old snowpack are difficult to recognise. Avalanches can in isolated cases penetrate deep layers and reach quite a large size. <br/> Backcountry touring calls for extensive experience in the assessment of avalanche danger and careful route selection. A latent danger of gliding avalanches exists. Areas with glide cracks are to be avoided as far as possible. As a consequence of a moderate to strong northerly wind, clearly visible wind slabs formed especially adjacent to ridgelines. This also applies in gullies and bowls below the tree line. The fresh wind slabs are lying on soft layers in all aspects. The various wind slabs have bonded poorly together. <br/> Faceted weak layers exist in the centre of the snowpack in particular above the tree line. <br/> Towards its base, the snowpack is moist and its surface has a melt-freeze crust, in particular at low and intermediate altitudes. A latent danger of gliding avalanches exists. As a consequence of low temperatures the snowpack can not consolidate, especially in the vicinity of peaks and at high altitude. Fresh wind slabs are to be evaluated with care and prudence. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/aaf41996-a9e4-488f-bad0-62aa48a784c8.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-14?region=aaf41996-a9e4-488f-bad0-62aa48a784c8 2021-02-13T16:00:00Z 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Avalanche.report https://avalanche.report Sexten Dolomites Eastern Pfunderer Mountains Durreck Range Val Müstair Alps Western Rieserferner Mountains Langtaufers Western Deferegger Alps Schnals Ridge Ortler Range Southern Stubai Alps Ulten Valley Southern Zillertal Alps and High Tauern Eastern Nonsberger Alps Saldurn-Mastaun Ridge Northern Dolomites of Fiemme Texel Mountains Gröden Dolomites Sarntal Alps Prags Dolomites Western Pfunderer Mountains considerable 2000 no_rating no_rating moderate 2000 no_rating no_rating dp6 dp2 wind_drifted_snow SE SW E W NW S N NE 2000 considerable considerable 3 3 3 persistent_weak_layers SE SW E W NW S N NE 2000 moderate moderate 3 3 1 gliding_snow SE SW E W S 2400 moderate moderate 1 2 steady 2021-02-14T23:00:00Z 2021-02-15T23:00:00Z Fresh wind slabs represent the main danger. At elevated altitudes a considerable avalanche danger will still be encountered. The fresh wind slabs can be released easily. or in isolated cases naturally, in all aspects above approximately 2000 m. The number and size of avalanche prone locations will increase with altitude. Avalanches can also penetrate deep layers and reach dangerously large size. Weak layers in the old snowpack can still be released in some places by individual winter sport participants in particular in areas where the snow cover is rather shallow. <br/> A latent danger of gliding avalanches exists. Areas with glide cracks are to be avoided as far as possible. As a consequence of a moderate to strong northerly wind, clearly visible wind slabs formed, especially adjacent to ridgelines and in gullies and bowls above the tree line. The various wind slabs have bonded poorly together. <br/> Faceted weak layers exist in the centre of the snowpack in particular above the tree line. This applies in all aspects. <br/> Towards its base, the snowpack is moist and its surface has a melt-freeze crust, in particular at low and intermediate altitudes. The weather will be cold. As a consequence of low temperatures and the occasionally strong wind, the snowpack can not consolidate during the next few days. Fresh wind slabs require caution. In addition a latent danger of gliding avalanches exists. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/585ac5d1-95a3-4ae3-b514-9fab2a334110.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-14?region=585ac5d1-95a3-4ae3-b514-9fab2a334110 2021-02-13T16:00:00Z 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Avalanche.report https://avalanche.report Weißkugel Range Western Verwall Mountains Gurgler Range Central Stubai Alps Eastern Verwall Mountains Northern Zillertal Alps Allgäu Alps Silvretta Venediger Range Samnaun Mountains Eastern Lechtal Alps - Ammergau Alps Northern Oetz and Stubai Alps Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Western Lechtal Alps Central Lechtal Alps Glockturm Range Grieskogel Mountains considerable treeline no_rating no_rating low treeline no_rating no_rating dp6 dp7 wind_drifted_snow SE E SW W NW S N NE treeline considerable considerable 2 3 3 persistent_weak_layers E W NW N NE 2000 moderate moderate 3 2 2 steady 2021-02-14T23:00:00Z 2021-02-15T23:00:00Z Wind slabs and weakly bonded old snow require caution. As a consequence of a sometimes strong wind from variable directions, easily released wind slabs formed. These can be released, even by a single winter sport participant and reach medium size. The avalanche prone locations are to be found in all aspects above the tree line. Avalanches can in isolated cases penetrate deep layers and reach large size. <br/> Avalanches can be released in the weakly bonded old snow especially at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. This applies in particular above approximately 2000 m on steep west, north and east facing slopes. Between approximately 2000 and 2400 m the avalanche prone locations are more prevalent. The fresh and older wind slabs are lying on soft layers at high altitudes and in high Alpine regions. <br/> Avalanche prone weak layers exist in the centre of the snowpack, especially between approximately 2000 and 2400 m on steep west, north and east facing slopes. Hardly any decrease in avalanche danger. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/2090ea99-2088-45e9-94ff-46c5fd3e8864.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-14?region=2090ea99-2088-45e9-94ff-46c5fd3e8864 2021-02-13T16:00:00Z 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Avalanche.report https://avalanche.report Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Eastern Rieserferner Mountains moderate treeline no_rating no_rating low treeline no_rating no_rating dp6 wind_drifted_snow SE E SW W NW S N NE treeline moderate moderate 2 3 2 steady 2021-02-14T23:00:00Z 2021-02-15T23:00:00Z Fresh wind slabs represent the main danger. As a consequence of a sometimes strong wind from variable directions, easily released wind slabs formed, especially adjacent to ridgelines and in gullies and bowls above the tree line. These can be released, even by a single winter sport participant and reach medium size. Avalanches can in isolated cases penetrate deep layers and reach large size. <br/> A latent danger of gliding avalanches exists. Areas with glide cracks are to be avoided as far as possible. The various wind slabs have bonded poorly together. <br/> Faceted weak layers exist in the centre of the snowpack in particular above the tree line. This applies in all aspects. <br/> Towards its base, the snowpack is moist and its surface has a melt-freeze crust, in particular at low and intermediate altitudes. Hardly any decrease in avalanche danger. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-14/2021-02-13_16-00-00/a283039b-1a9f-46b8-b6fd-fa131380989a.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-14?region=a283039b-1a9f-46b8-b6fd-fa131380989a 2021-02-13T16:00:00Z 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Avalanche.report https://avalanche.report Karwendel Mountains Brandenberg Alps Western Kitzbühel Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps moderate 1800 no_rating no_rating low 1800 no_rating no_rating dp6 wind_drifted_snow SE E SW W NW S N NE 1800 moderate moderate 2 3 2 steady 2021-02-14T23:00:00Z 2021-02-15T23:00:00Z Fresh wind slabs require caution. As a consequence of a sometimes strong wind, avalanche prone wind slabs formed. The avalanche prone locations are to be found in particular adjacent to ridgelines. Such avalanche prone locations are clearly recognisable to the trained eye. <br/> Weak layers in the old snowpack can still be released in very isolated cases by individual winter sport participants. This applies at high altitude, in particular in the Western Kitzbühel Alps. In some cases the various wind slabs have bonded still only poorly together. Individual weak layers exist in the centre of the snowpack. At low altitude a little snow is lying. Hardly any decrease in avalanche danger.