link Link to website https://avalanche.report/bulletin/2022-01-16 simple_link Link to the simplified website https://avalanche.report/simple/2022-01-16/en.html fd_albina_map.jpg Danger rating map (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_albina_map.jpg fd_tyrol_map.jpg Danger rating map Tirol (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_tyrol_map.jpg fd_southtyrol_map.jpg Danger rating map Southtyrol (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_southtyrol_map.jpg fd_trentino_map.jpg Danger rating map Trentino (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_trentino_map.jpg pdf PDF https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/2022-01-16_en.pdf tyrol_pdf PDF Tirol https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/2022-01-16_AT-07_en.pdf southtyrol_pdf PDF Southtyrol https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/2022-01-16_IT-32-BZ_en.pdf trentino_pdf PDF Trentino https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/2022-01-16_IT-32-TN_en.pdf fd_overlay.png Danger rating overlay (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_overlay.png fd_regions.json GeoJSON for regions (whole day) https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/fd_regions.json dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2022-01-16/2022-01-15_16-00-00/1f68ce7b-ec71-4d57-a63d-3aac6884cd7b.jpg website Link to region on the website https://avalanche.report/bulletin/2022-01-16?region=1f68ce7b-ec71-4d57-a63d-3aac6884cd7b 2022-01-15T16:00:00.006Z 2022-01-15T23:00:00Z 2022-01-16T23:00:00Z Avalanche.report https://avalanche.report Sexten Dolomites Latemar Southern Adamello Adamello - Presanella Northern Brenta - Peller Bondone and Stivo Folgaria - Laverone Southern Brenta Southern Lagorai Northern Lagorai Allgäu Alps Eastern Lechtal Alps - Ammergau Alps Mieming Mountains Karwendel Mountains Brandenberg Alps Wilder Kaiser Mountains - Waidring 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 Kitzbühel Alps Western Pfunderer Mountains Eastern Kitzbühel Alps Glockturm Range Maddalene Pine' - Mocheni Valley 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 Nonsberger Alps Eastern Rieserferner Mountains Northern Dolomites of Fiemme Glockner Range Gröden Dolomites Primiero - Pale di S. Martino Eastern Deferegger Alps Prags Dolomites Prealps Schober Mountains Cembra Valley Lienzer Dolomites Vallarsa Western Nonsberg Alps Fassa Valley Sole, Pejo and Rabbi Ledro Valley Paganella Marzola - Valsugana low no_rating no_rating dp7 dp4 increasing 2022-01-16T23:00:00Z 2022-01-17T23:00:00Z A generally favourable avalanche situation will prevail. The avalanche prone locations are to be found on very steep shady slopes above approximately 2400 m and in gullies and bowls, and behind abrupt changes in the terrain. In very isolated cases avalanches can be triggered in the faceted old snow and reach medium size. Caution is to be exercised 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/> 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. The spring-like weather conditions gave rise to increasing consolidation of the snowpack. Field observations and stability tests confirm good snowpack stability. <br/> The old wind slabs have bonded well with the old snowpack. They are in individual cases still prone to triggering. In very isolated cases weak layers exist in the centre of the snowpack. This applies in particular on very steep shady slopes above approximately 2400 m. <br/> At elevated altitudes snow depths vary greatly, depending on the infuence of the wind. On sunny slopes below approximately 2200 m only a little snow is lying. As a consequence of a sometimes strong wind from northerly directions, mostly small wind slabs will form on Monday at elevated altitudes. In the north and in the regions with a lot of snow the wind slabs are larger.