link Link to website https://avalanche.report/bulletin/2021-02-13 simple_link Link to the simplified website https://avalanche.report/simple/2021-02-13/en.html fd_albina_map.jpg Danger rating map (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_albina_map.jpg fd_tyrol_map.jpg Danger rating map Tirol (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_tyrol_map.jpg fd_southtyrol_map.jpg Danger rating map Southtyrol (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_southtyrol_map.jpg fd_trentino_map.jpg Danger rating map Trentino (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_trentino_map.jpg pdf PDF https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/2021-02-13_en.pdf tyrol_pdf PDF Tirol https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/2021-02-13_AT-07_en.pdf southtyrol_pdf PDF Southtyrol https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/2021-02-13_IT-32-BZ_en.pdf trentino_pdf PDF Trentino https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/2021-02-13_IT-32-TN_en.pdf fd_overlay.png Danger rating overlay (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_overlay.png fd_regions.json GeoJSON for regions (whole day) https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/fd_regions.json dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-02-13/2021-02-12_16-00-00/162f37f4-ff92-4075-831c-79cce72f5710.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-13?region=162f37f4-ff92-4075-831c-79cce72f5710 2021-02-12T16:00:00Z 2021-02-12T23:00:00Z 2021-02-13T23:00:00Z 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 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z 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/2021-02-13/2021-02-12_16-00-00/0bef310d-12f2-46b9-a94f-2fb6a45a6809.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-13?region=0bef310d-12f2-46b9-a94f-2fb6a45a6809 2021-02-12T16:00:00Z 2021-02-12T23:00:00Z 2021-02-13T23:00:00Z Avalanche.report https://avalanche.report Sexten Dolomites Val Müstair Alps Langtaufers Schnals Ridge Southern Stubai Alps Southern Zillertal Alps and High Tauern Saldurn-Mastaun Ridge Texel Mountains Sarntal Alps Western Pfunderer Mountains Eastern Pfunderer Mountains Durreck Range Western Rieserferner Mountains Western Deferegger Alps Ortler Range Ulten Valley Venediger Range Eastern Nonsberger Alps Eastern Rieserferner Mountains Northern Dolomites of Fiemme Glockner Range Gröden Dolomites Eastern Deferegger Alps Prags Dolomites Schober Mountains Lienzer Dolomites 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 gliding_snow SE SW E W S 2400 moderate moderate 1 2 persistent_weak_layers SE SW E W NW S N NE 2000 moderate moderate 3 3 1 steady 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Wind slabs in the high Alpine regions. Gliding snow is to be evaluated with care and prudence. 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. The fresh wind slabs are lying on soft layers in all aspects above the tree line. The various wind slabs have bonded poorly together. <br/> Towards its base, the snowpack is moist and its surface has a melt-freeze crust, in particular at low and intermediate altitudes. <br/> Avalanche prone weak layers exist in the centre of the snowpack in all aspects, in particular above approximately 2000 m. 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/2021-02-13/2021-02-12_16-00-00/84be6ea6-79f2-4710-bbad-e946e6abe83a.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-13?region=84be6ea6-79f2-4710-bbad-e946e6abe83a 2021-02-12T16:00:00Z 2021-02-12T23:00:00Z 2021-02-13T23:00:00Z Avalanche.report https://avalanche.report Gurgler Range 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 3 3 3 persistent_weak_layers E W NW N NE 2000 moderate moderate 3 2 2 steady 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Wind slabs are to be evaluated critically. As a consequence of a sometimes strong wind from variable directions, easily released wind slabs will form. These can over a wide area be released, even by a single winter sport participant. As a consequence of the strong wind individual natural avalanches are possible. The avalanche prone locations are to be found in all aspects at high altitudes and in high Alpine regions. Avalanches can be released in the weakly bonded old snow especially on west, north and east facing slopes. This applies in particular above approximately 2000 m. Between approximately 2000 and 2400 m the avalanche prone locations are more prevalent. <br/> In isolated cases avalanches can penetrate deep layers and reach large size. The fresh 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 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/2021-02-13/2021-02-12_16-00-00/8c794578-0fde-440e-ae5d-377294ea6ebe.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-13?region=8c794578-0fde-440e-ae5d-377294ea6ebe 2021-02-12T16:00:00Z 2021-02-12T23:00:00Z 2021-02-13T23:00:00Z Avalanche.report https://avalanche.report Weißkugel Range Western Verwall Mountains Central Stubai Alps Eastern Verwall Mountains Northern Zillertal Alps Allgäu Alps Silvretta 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 2000 no_rating no_rating low 2000 no_rating no_rating dp6 dp7 persistent_weak_layers E W NW N NE 2000 considerable considerable 3 3 2 wind_drifted_snow SE E SW W NW S N NE treeline moderate moderate 2 3 2 steady 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Wind slabs and weakly bonded old snow are to be assessed with care and prudence. 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. <br/> As a consequence of a sometimes strong wind from variable directions, easily released wind slabs will form. 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. The fresh 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/2021-02-13/2021-02-12_16-00-00/7c0d6c3c-1a15-4ab7-b895-8a885b97f18b.jpg website Link to region on the website https://avalanche.report/bulletin/2021-02-13?region=7c0d6c3c-1a15-4ab7-b895-8a885b97f18b 2021-02-12T16:00:00Z 2021-02-12T23:00:00Z 2021-02-13T23:00:00Z 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 2021-02-13T23:00:00Z 2021-02-14T23:00:00Z Fresh wind slabs require caution. As a consequence of a sometimes strong wind, avalanche prone wind slabs will form. 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.