link Link to website https://avalanche.report/bulletin/2021-01-09 simple_link Link to the simplified website https://avalanche.report/simple/2021-01-09/en.html fd_albina_map.jpg Danger rating map (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_albina_map.jpg fd_tyrol_map.jpg Danger rating map Tirol (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_tyrol_map.jpg fd_southtyrol_map.jpg Danger rating map Southtyrol (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_southtyrol_map.jpg fd_trentino_map.jpg Danger rating map Trentino (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_trentino_map.jpg pdf PDF https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/2021-01-09_en.pdf tyrol_pdf PDF Tirol https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/2021-01-09_AT-07_en.pdf southtyrol_pdf PDF Southtyrol https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/2021-01-09_IT-32-BZ_en.pdf trentino_pdf PDF Trentino https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/2021-01-09_IT-32-TN_en.pdf fd_overlay.png Danger rating overlay (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_overlay.png fd_regions.json GeoJSON for regions (whole day) https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd_regions.json dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/fd807858-5dd7-46ec-9690-d9d018d664e2.jpg website Link to region on the website https://avalanche.report/bulletin/2021-01-09?region=fd807858-5dd7-46ec-9690-d9d018d664e2 2021-01-08T16:00:00Z 2021-01-08T23:00:00Z 2021-01-09T23:00:00Z Avalanche.report https://avalanche.report Sexten Dolomites Eastern Pfunderer Mountains Durreck Range Western Rieserferner Mountains Western Deferegger Alps Ortler Range Schnals Ridge Southern Stubai Alps Ulten Valley Venediger Range Southern Zillertal Alps and High Tauern Eastern Nonsberger Alps Eastern Rieserferner Mountains Northern Dolomites of Fiemme Saldurn-Mastaun Ridge Glockner Range Gröden Dolomites Texel Mountains Eastern Deferegger Alps Prags Dolomites Sarntal Alps Schober Mountains Western Pfunderer Mountains Lienzer Dolomites considerable treeline no_rating no_rating moderate treeline no_rating no_rating dp8 dp4 persistent_weak_layers N SE S NW SW E W NE treeline considerable considerable 2 3 3 wind_drifted_snow N NW SE S SW E W NE treeline moderate moderate 2 3 2 persistent_weak_layers N NW W E NE treeline moderate moderate 2 2 2 steady 2021-01-09T23:00:00Z 2021-01-10T23:00:00Z A treacherous avalanche situation will prevail. Weak layers in the upper part of the snowpack necessitate caution. The near-surface layers of the snowpack necessitate caution and restraint. Dry avalanches can be triggered in the weakly bonded old snow and reach quite a large size. Remotely triggered avalanches are possible. Avalanche prone locations for dry avalanches are to be found on steep shady slopes, also below the tree line. The avalanche prone locations are covered with new snow and are barely recognisable, even to the trained eye. Especially places where surface hoar has been covered with snow are treacherous. Whumpfing sounds and the formation of shooting cracks when stepping on the snowpack serve as an alarm indicating the danger. Meticulous route selection is important. <br/> The fresh wind slabs are mostly small but prone to triggering. These avalanche prone locations are to be found above the tree line, caution is to be exercised adjacent to ridgelines and in gullies and bowls. <br/> As a consequence of solar radiation more dry snow slides and avalanches are possible as the day progresses. <br/> In addition a latent danger of gliding avalanches exists. Faceted weak layers exist in the top section of the snowpack. The fresh wind slabs will be deposited on soft layers. The somewhat older wind slabs are lying on surface hoar in some places. Stability tests and snow profiles confirm the unfavourable bonding of the snowpack. As a consequence of low temperatures the snowpack can not consolidate. <br/> Towards its base, the snowpack is well consolidated. A precarious avalanche situation will persist. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/291701ab-7200-45a9-9586-56b81b1ff47b.jpg website Link to region on the website https://avalanche.report/bulletin/2021-01-09?region=291701ab-7200-45a9-9586-56b81b1ff47b 2021-01-08T16:00:00Z 2021-01-08T23:00:00Z 2021-01-09T23:00:00Z 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 1600 no_rating no_rating moderate 1600 no_rating no_rating persistent_weak_layers N SE S NW SW E W NE 1600 considerable considerable 3 3 3 persistent_weak_layers N SE S NW SW E W NE 1600 moderate moderate 2 2 3 wind_drifted_snow N SE S NW SW E W NE treeline considerable considerable 3 3 3 steady 2021-01-09T23:00:00Z 2021-01-10T23:00:00Z Weak layers in the upper part of the snowpack necessitate caution. Dry avalanches can as before be released, even by small loads in isolated cases and reach large size. Small and medium-sized natural avalanches are, however, not entirely ruled out. The avalanche prone locations are to be found in particular adjacent to ridgelines and in gullies and bowls, caution is to be exercised on steep slopes also below the tree line, as well as at the base of rock walls and behind abrupt changes in the terrain. <br/> Whumpfing sounds and the formation of shooting cracks when stepping on the snowpack are a clear indication of a weakly bonded snowpack. Remotely triggered avalanches are possible. In addition a latent danger of gliding avalanches exists. In the event of solar radiation this applies in particular on steep sunny slopes. <br/> Ski touring and snowshoe hiking call for extensive experience in the assessment of avalanche danger and careful route selection. Towards its surface, the snowpack is fairly homogeneous; its surface consists of loosely bonded snow. In some places new snow and wind slabs are lying on surface hoar. The avalanche prone locations are sometimes covered with new snow and are therefore difficult to recognise. The new snow and wind slabs of last week are bonding only slowly with the old snowpack in all aspects. <br/> Faceted weak layers exist in the centre of the snowpack in particular on shady slopes. Towards its base, the snowpack is well consolidated. At elevated altitudes a precarious avalanche situation will still be encountered. As a consequence of low temperatures the snowpack can not consolidate. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/022b2805-677d-48cc-931b-80337bf016c3.jpg website Link to region on the website https://avalanche.report/bulletin/2021-01-09?region=022b2805-677d-48cc-931b-80337bf016c3 2021-01-08T16:00:00Z 2021-01-08T23:00:00Z 2021-01-09T23:00:00Z Avalanche.report https://avalanche.report Gurgler Range Central Stubai Alps Northern Zillertal Alps moderate 2000 no_rating no_rating low 2000 no_rating no_rating dp4 dp8 persistent_weak_layers N SE S NW SW E W NE 2000 moderate moderate 2 2 2 wind_drifted_snow N NW W E NE 2600 moderate moderate 2 2 2 steady 2021-01-09T23:00:00Z 2021-01-10T23:00:00Z The current avalanche situation calls for experience in the assessment of avalanche danger. A sometimes treacherous avalanche situation will prevail. This applies in particular in the south. Weak layers in the upper part of the snowpack can still be released in some place by winter sport participants in particular on steep sunny slopes. This applies in particular between approximately 2200 and 2600 m. Mostly the avalanches are medium-sized. <br/> Also places where surface hoar has been covered with snow are unfavourable. Caution is to be exercised in particular on very steep shady slopes at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example, also at intermediate altitudes. Faceted weak layers exist in the top section of the snowpack. This applies in particular on sunny slopes between approximately 2200 and 2600 m. The older wind slabs are lying on surface hoar in some places. Towards its base, the snowpack is well consolidated. Weak layers in the upper part of the snowpack necessitate caution. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/e7cfab4c-6b51-4472-bf10-0a233e2b8b3c.jpg website Link to region on the website https://avalanche.report/bulletin/2021-01-09?region=e7cfab4c-6b51-4472-bf10-0a233e2b8b3c 2021-01-08T16:00:00Z 2021-01-08T23:00:00Z 2021-01-09T23:00:00Z Avalanche.report https://avalanche.report Weißkugel Range Val Müstair Alps Western Verwall Mountains Langtaufers Eastern Verwall Mountains Allgäu Alps Silvretta Samnaun Mountains Eastern Lechtal Alps - Ammergau Alps Northern Oetz and Stubai Alps Mieming Mountains Western Tuxer Alps Karwendel Mountains Eastern Tuxer Alps Western Lechtal Alps Central Lechtal Alps Glockturm Range Grieskogel Mountains moderate treeline no_rating no_rating low treeline no_rating no_rating dp1 dp7 wind_drifted_snow N NW SE S SW W E NE treeline moderate moderate 2 2 2 persistent_weak_layers N NW W E NE 2400 moderate moderate 2 2 2 steady 2021-01-09T23:00:00Z 2021-01-10T23:00:00Z Individual avalanche prone locations for dry avalanches are to be found on very steep slopes above approximately 2200 m. Weak layers in the lower part of the snowpack can be released by large additional loads. This applies in particular on very steep shady slopes above approximately 2200 m, as well as at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. Mostly the avalanches are medium-sized. <br/> Fresh and somewhat older wind slabs are mostly shallow but in some cases prone to triggering. Caution is to be exercised in particular adjacent to ridgelines and in gullies and bowls. Here only a little snow is lying. The snowpack is faceted. The fresh and somewhat older wind slabs are lying on top of a weakly bonded old snowpack. Faceted weak layers exist in the bottom section of the snowpack at high altitudes and in high Alpine regions. The avalanche danger will persist. dangerRatingMap Simplified danger rating map of the region https://avalanche.report/albina_files/2021-01-09/2021-01-08_16-00-00/38404b85-368a-405c-8d86-a93790454da9.jpg website Link to region on the website https://avalanche.report/bulletin/2021-01-09?region=38404b85-368a-405c-8d86-a93790454da9 2021-01-08T16:00:00Z 2021-01-08T23:00:00Z 2021-01-09T23:00:00Z Avalanche.report https://avalanche.report Brandenberg Alps Western Kitzbühel Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps low no_rating no_rating steady 2021-01-09T23:00:00Z 2021-01-10T23:00:00Z Low, level 1. Individual avalanche prone locations for dry avalanches are to be found on very steep shady slopes above approximately 2000 m, especially adjacent to ridgelines. The avalanche prone locations are rare and are easy to recognise. From a snow sport perspective, in most cases insufficient snow is lying. Hardly any weak layers exist in the snowpack. Low, level 1.