linkLink to websitehttps://avalanche.report/bulletin/2019-02-19simple_linkLink to the simplified websitehttps://avalanche.report/simple/2019-02-19/en.htmlfd_albina_map.jpgDanger rating map (whole day)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/fd_albina_map.jpgfd_tyrol_map.jpgDanger rating map Tirol (whole day)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/fd_tyrol_map.jpgfd_southtyrol_map.jpgDanger rating map Southtyrol (whole day)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/fd_southtyrol_map.jpgfd_trentino_map.jpgDanger rating map Trentino (whole day)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/fd_trentino_map.jpgpdfPDF https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/2019-02-19_en.pdftyrol_pdfPDF Tirolhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/2019-02-19_AT-07_en.pdfsouthtyrol_pdfPDF Southtyrolhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/2019-02-19_IT-32-BZ_en.pdftrentino_pdfPDF Trentinohttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/2019-02-19_IT-32-TN_en.pdfam_albina_map.jpgDanger rating map (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_albina_map.jpgam_tyrol_map.jpgDanger rating map Tirol (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_tyrol_map.jpgam_southtyrol_map.jpgDanger rating map Southtyrol (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_southtyrol_map.jpgam_trentino_map.jpgDanger rating map Trentino (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_trentino_map.jpgpm_albina_map.jpgDanger rating map (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_albina_map.jpgpm_tyrol_map.jpgDanger rating map Tirol (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_tyrol_map.jpgpm_southtyrol_map.jpgDanger rating map Southtyrol (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_southtyrol_map.jpgpm_trentino_map.jpgDanger rating map Trentino (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_trentino_map.jpgam_overlay.pngDanger rating overlay (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_overlay.pngpm_overlay.pngDanger rating overlay (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_overlay.pngam_regions.jsonGeoJSON for regions (AM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/am_regions.jsonpm_regions.jsonGeoJSON for regions (PM)https://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/pm_regions.jsondangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/43360506-480b-46b6-95a7-b062589567b0.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=43360506-480b-46b6-95a7-b062589567b02019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZEastern Deferegger AlpsSchober MountainsLienzer DolomitesSexten DolomitesEastern Pfunderer MountainsDurreck RangeWestern Rieserferner MountainsVal Müstair AlpsWestern Deferegger AlpsLangtaufersOrtler RangeSchnals RidgeSouthern Stubai AlpsSouthern Zillertal Alps and High TauernSaldurn-Mastaun RidgeTexel MountainsPrags DolomitesWestern Pfunderer Mountainsmoderatemoderate222moderate12dp2dp1persistent_weak_layersNENNW18002600gliding_snowNESNESWNWSEW2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZIncrease in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase in particular on steep sunny slopes below approximately 2600 m. Medium-sized gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load. Weak layers in the old snowpack can be released in isolated cases and mostly by large additional loads also on very steep sunny slopes, in particular in the afternoon.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/43360506-480b-46b6-95a7-b062589567b0_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=43360506-480b-46b6-95a7-b062589567b02019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZEastern Deferegger AlpsSchober MountainsLienzer DolomitesSexten DolomitesEastern Pfunderer MountainsDurreck RangeWestern Rieserferner MountainsVal Müstair AlpsWestern Deferegger AlpsLangtaufersOrtler RangeSchnals RidgeSouthern Stubai AlpsSouthern Zillertal Alps and High TauernSaldurn-Mastaun RidgeTexel MountainsPrags DolomitesWestern Pfunderer Mountainsmoderatemoderate222moderate12dp2dp1gliding_snowNESNSWENWWSE2600wet_snowSSWSE2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZIncrease in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase in particular on steep sunny slopes below approximately 2600 m. Medium-sized gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load. Weak layers in the old snowpack can be released in isolated cases and mostly by large additional loads also on very steep sunny slopes, in particular in the afternoon.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/cc563ea8-674e-43ba-ad46-7405791fbcc9.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=cc563ea8-674e-43ba-ad46-7405791fbcc92019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZGlockner RangeEastern Rieserferner Mountainslowlow221low11dp2dp1gliding_snowNESNESWNWSEW2600persistent_weak_layersNENNW18002600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase in particular on steep sunny slopes below approximately 2600 m. Large gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load. Weak layers in the old snowpack can be released in isolated cases and mostly by large additional loads also on very steep sunny slopes, in particular in the afternoon.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/cc563ea8-674e-43ba-ad46-7405791fbcc9_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=cc563ea8-674e-43ba-ad46-7405791fbcc92019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZGlockner RangeEastern Rieserferner Mountainslowlow221low11dp2dp1gliding_snowNESNSWENWWSE2600wet_snowSSWSE2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase in particular on steep sunny slopes below approximately 2600 m. Large gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load. Weak layers in the old snowpack can be released in isolated cases and mostly by large additional loads also on very steep sunny slopes, in particular in the afternoon.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/8049dc6d-49de-4bdc-ae24-9b7c5a78dd23.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=8049dc6d-49de-4bdc-ae24-9b7c5a78dd232019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZGröden DolomitesSarntal AlpsUlten Valleymoderatemoderate222moderate12dp2dp1persistent_weak_layersNENNW1800gliding_snowNESNESWNWSEW2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZIncrease in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches and moist snow slides being released will increase in particular on steep sunny slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/8049dc6d-49de-4bdc-ae24-9b7c5a78dd23_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=8049dc6d-49de-4bdc-ae24-9b7c5a78dd232019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZGröden DolomitesSarntal AlpsUlten Valleymoderatemoderate222moderate12dp2dp1persistent_weak_layersNENNW1800wet_snowSSWSE2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZIncrease in danger of gliding avalanches and wet snow slides as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution.A latent danger of gliding avalanches exists. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches and moist snow slides being released will increase in particular on steep sunny slopes below approximately 2600 m. Weak layers near the ground can still be released in isolated cases especially on very steep shady slopes, this applies in particular in case of a large load.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Isolated avalanche prone weak layers exist in the old snowpack.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/b5954506-4919-4e6d-abf2-5d2c07bd28af.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=b5954506-4919-4e6d-abf2-5d2c07bd28af2019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZSouthern AdamelloPrimiero - Pale di S. MartinoAdamello - PresanellaNorthern Brenta - PellerSouthern BrentaFassa ValleySole, Pejo and RabbiSouthern LagoraiNorthern LagoraiLatemarMaddalenePine' - Mocheni Valleymoderatelow211moderate21dp10persistent_weak_layersNENENWWtreelinefavourable_situationtreelinesteady2019-02-19T23:00:00Z2019-02-20T23:00:00ZWeak layers in the lower part of the snowpack necessitate caution and restraint. As a consequence of warming during the day and solar radiation the prevalence of avalanche prone locations will increase in the afternoon.The wind slabs have bonded quite well with the old snowpack in particular on steep sunny slopes. These can be released, especially by large additional loads,. Faceted weak layers exist in the bottom section of the old snowpack especially on steep west, north and east facing slopes. The avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack and in gullies and bowls, and behind abrupt changes in the terrain. A clear night will be followed in the early morning by quite favourable conditions generally, but the avalanche danger will increase later. Moist avalanches can in isolated cases penetrate near-ground layers of the snowpack and reach large size in particular on sunny slopes. Backcountry tours and off-piste skiing should be started very early and concluded timely.The snowpack will become well bonded until the early morning. The surface of the snowpack will freeze, but a strong crust will not form and will soften during the day. The fresh and older wind slabs are lying on the unfavourable surface of an old snowpack in particular on extremely steep, rather lightly snow-covered shady slopes. Faceted weak layers exist in the bottom section of the snowpack in particular here.As a consequence of warming during the day and the solar radiation, the likelihood of moist loose snow avalanches being released will increase gradually in particular on rocky sunny slopes below approximately 2500 m.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/b5954506-4919-4e6d-abf2-5d2c07bd28af_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=b5954506-4919-4e6d-abf2-5d2c07bd28af2019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZSouthern AdamelloPrimiero - Pale di S. MartinoAdamello - PresanellaNorthern Brenta - PellerSouthern BrentaFassa ValleySole, Pejo and RabbiSouthern LagoraiNorthern LagoraiLatemarMaddalenePine' - Mocheni Valleymoderatelow211moderate21dp10wet_snowSSWSEW2600favourable_situationtreelinesteady2019-02-19T23:00:00Z2019-02-20T23:00:00ZWeak layers in the lower part of the snowpack necessitate caution and restraint. As a consequence of warming during the day and solar radiation the prevalence of avalanche prone locations will increase in the afternoon.The wind slabs have bonded quite well with the old snowpack in particular on steep sunny slopes. These can be released, especially by large additional loads,. Faceted weak layers exist in the bottom section of the old snowpack especially on steep west, north and east facing slopes. The avalanche prone locations are to be found in particular at transitions from a shallow to a deep snowpack and in gullies and bowls, and behind abrupt changes in the terrain. A clear night will be followed in the early morning by quite favourable conditions generally, but the avalanche danger will increase later. Moist avalanches can in isolated cases penetrate near-ground layers of the snowpack and reach large size in particular on sunny slopes. Backcountry tours and off-piste skiing should be started very early and concluded timely.The snowpack will become well bonded until the early morning. The surface of the snowpack will freeze, but a strong crust will not form and will soften during the day. The fresh and older wind slabs are lying on the unfavourable surface of an old snowpack in particular on extremely steep, rather lightly snow-covered shady slopes. Faceted weak layers exist in the bottom section of the snowpack in particular here.As a consequence of warming during the day and the solar radiation, the likelihood of moist loose snow avalanches being released will increase gradually in particular on rocky sunny slopes below approximately 2500 m.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/ae4d3b39-5a14-441f-8e99-9ca22d07520c.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=ae4d3b39-5a14-441f-8e99-9ca22d07520c2019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZWestern Tuxer AlpsEastern Tuxer AlpsCentral Stubai AlpsNorthern Zillertal Alpslowlow221low11dp2dp10gliding_snowNESNSWENWSEW2600persistent_weak_layersNENNW22002600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches as a consequence of warming during the day and solar radiation.A substantial danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase further in particular on steep sunny slopes below approximately 2600 m. Large and very large gliding avalanches are possible. There is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Dry avalanches can additionally in very isolated cases be released in near-ground layers by large loads. This applies on very steep shady slopes between approximately 2200 and 2600 m in areas where the snow cover is rather shallow.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Faceted weak layers exist deep in the old snowpack, in particular on shady slopes between approximately 2200 and 2600 m.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/ae4d3b39-5a14-441f-8e99-9ca22d07520c_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=ae4d3b39-5a14-441f-8e99-9ca22d07520c2019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZWestern Tuxer AlpsEastern Tuxer AlpsCentral Stubai AlpsNorthern Zillertal Alpslowlow211low11dp2dp10gliding_snowNESNSWENWWSE2600wet_snowSSWSE2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches as a consequence of warming during the day and solar radiation.A substantial danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase further in particular on steep sunny slopes below approximately 2600 m. Large and very large gliding avalanches are possible. There is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m. Dry avalanches can additionally in very isolated cases be released in near-ground layers by large loads. This applies on very steep shady slopes between approximately 2200 and 2600 m in areas where the snow cover is rather shallow.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. Faceted weak layers exist deep in the old snowpack, in particular on shady slopes between approximately 2200 and 2600 m.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/d51c5781-93bc-4670-aea1-7e418f01df74.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=d51c5781-93bc-4670-aea1-7e418f01df742019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZWeißkugel RangeWestern Verwall MountainsGurgler RangeEastern Verwall MountainsAllgäu AlpsSilvrettaVenediger RangeSamnaun MountainsEastern Lechtal Alps - Ammergau AlpsNorthern Oetz and Stubai AlpsMieming MountainsKarwendel MountainsBrandenberg AlpsWestern Kitzbühel AlpsWilder Kaiser Mountains - Waidring AlpsEastern Kitzbühel AlpsWestern Lechtal AlpsCentral Lechtal AlpsGlockturm RangeGrieskogel Mountainslowlow221low11dp2dp10gliding_snowNESNSWENWSEW2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches as a consequence of warming during the day and solar radiation.A substantial danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase further in particular on steep sunny slopes below approximately 2600 m. Large and very large gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. The old snowpack will be favourable.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/d51c5781-93bc-4670-aea1-7e418f01df74_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=d51c5781-93bc-4670-aea1-7e418f01df742019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZWeißkugel RangeWestern Verwall MountainsGurgler RangeEastern Verwall MountainsAllgäu AlpsSilvrettaVenediger RangeSamnaun MountainsEastern Lechtal Alps - Ammergau AlpsNorthern Oetz and Stubai AlpsMieming MountainsKarwendel MountainsBrandenberg AlpsWestern Kitzbühel AlpsWilder Kaiser Mountains - Waidring AlpsEastern Kitzbühel AlpsWestern Lechtal AlpsCentral Lechtal AlpsGlockturm RangeGrieskogel Mountainslowlow211low11dp2dp10gliding_snowNESNSWENWWSE2600wet_snowSSWSE2600decreasing2019-02-19T23:00:00Z2019-02-20T23:00:00ZSignificant increase in danger of gliding avalanches as a consequence of warming during the day and solar radiation.A substantial danger of gliding avalanches exists. This applies on steep grassy slopes. As a consequence of warming during the day and the solar radiation, the likelihood of gliding avalanches being released will increase further in particular on steep sunny slopes below approximately 2600 m. Large and very large gliding avalanches are possible. In addition there is a danger of wet loose snow avalanches. This applies in the afternoon, especially on extremely steep southeast, south and southwest facing slopes below approximately 2600 m.Outgoing longwave radiation during the night will be good. The surface of the snowpack has frozen to form a strong crust and will soften during the day. This applies at low altitude as well as on very steep sunny slopes in particular below approximately 2600 m. The old snowpack will be favourable.Slight decrease in danger of gliding avalanches and wet snow slides as the temperature drops.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/5403a057-73eb-4044-a77d-ffba619d6cde.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=5403a057-73eb-4044-a77d-ffba619d6cde2019-02-18T16:00:00Z2019-02-18T23:00:00Z2019-02-19T11:00:00ZEastern Nonsberger AlpsNorthern Dolomites of FiemmePrealpsCembra ValleyBondone and StivoVallarsaWestern Nonsberg AlpsFolgaria - LaveroneLedro ValleyPaganellaMarzola - Valsuganalowlow221low11dp10persistent_weak_layersNENNWtreelinefavourable_situationtreelinesteady2019-02-19T23:00:00Z2019-02-20T23:00:00ZSlight increase in avalanche danger as a consequence of warming during the day.A clear night will be followed in the early morning by quite favourable conditions generally. As a consequence of warming during the day and solar radiation there will be an increase in the danger of wet and gliding avalanches. Avalanches can in isolated cases be released by small loads and reach medium size. The avalanche prone locations are to be found at transitions from a shallow to a deep snowpack above the tree line. This applies in particular on steep shady slopes and adjacent to ridgelines and in gullies and bowls. Backcountry tours should be started and concluded early.The surface of the snowpack will freeze to form a strong crust and will soften during the day. Faceted weak layers exist in the bottom section of the snowpack in particular in shady places that are protected from the wind. Only a little snow is lying.A generally favourable avalanche situation will prevail.dangerRatingMapSimplified danger rating map of the regionhttps://avalanche.report/albina_files/2019-02-19/2019-02-18_16-00-00/5403a057-73eb-4044-a77d-ffba619d6cde_PM.jpgwebsiteLink to region on the websitehttps://avalanche.report/bulletin/2019-02-19?region=5403a057-73eb-4044-a77d-ffba619d6cde2019-02-18T16:00:00Z2019-02-19T11:00:00Z2019-02-19T23:00:00ZEastern Nonsberger AlpsNorthern Dolomites of FiemmePrealpsCembra ValleyBondone and StivoVallarsaWestern Nonsberg AlpsFolgaria - LaveroneLedro ValleyPaganellaMarzola - Valsuganamoderatemoderate232moderate12dp10persistent_weak_layersNENNWtreelinewet_snowSESWSEW2600steady2019-02-19T23:00:00Z2019-02-20T23:00:00ZSlight increase in avalanche danger as a consequence of warming during the day.A clear night will be followed in the early morning by quite favourable conditions generally. As a consequence of warming during the day and solar radiation there will be an increase in the danger of wet and gliding avalanches. Avalanches can in isolated cases be released by small loads and reach medium size. The avalanche prone locations are to be found at transitions from a shallow to a deep snowpack above the tree line. This applies in particular on steep shady slopes and adjacent to ridgelines and in gullies and bowls. Backcountry tours should be started and concluded early.The surface of the snowpack will freeze to form a strong crust and will soften during the day. Faceted weak layers exist in the bottom section of the snowpack in particular in shady places that are protected from the wind. Only a little snow is lying.A generally favourable avalanche situation will prevail.