2016-02-13T07:30:00+01:00 Rudi Mair 2016-02-13+01:00 https://lawine.tirol.gv.at/data/fotos/wind_15.jpg https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/colour/png/en https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/bw/png/en https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/detail/png/en https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem1/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem1_elevation/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem1_aspect/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem2/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem2_elevation/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/problem2_aspect/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/generallevel/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/generallevel_bw/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/resources/tendency/png https://lawine.tirol.gv.at/rest/bulletin/2016-02-13_073000/pdf/en Above 2200m, regionally considerable danger. Beware fresh, small snowdrift accumulations 2016-02-10+01:00 3 2016-02-11+01:00 3 2016-02-12+01:00 3 2016-02-13+01:00 3 2016-02-14+01:00 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2400 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2400 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2400 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2400 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2400 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2400 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2400 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2400 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 1 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 1 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 1 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 1 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 2200 2 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 3 2016-02-13T00:00:00+01:00 2016-02-13T11:59:59+01:00 1800 1 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 3 2016-02-13T12:00:00+01:00 2016-02-13T23:59:59+01:00 1800 1 DP6 DP1 DP7 drifting snow 2200 fresh, small persistent weak layer 2200 shady zones Alpine Weather Forecast (ZAMG-Weather Service Innsbruck) Weather: A low pressure zone over northern and central Europe is the dominant factor, Tirol lies at its edge in the path of a variable westerly air current. Today, barrier clouds in northern regions to start with, sunny in East Tirol; then, increasingly, a foehn scenario will arise from the south. Mountain weather today: in the Northern Alps light foehn winds, becoming ever sunnier. On the Main Alpine Ridge and, even more, in the Dolomites, sunshine all day. By evening, cloud will move in above summit altitude. Temperature at 2000m, -1 degree; at 3000m, -10 degrees. Winds will be westerly, initially blowing at brisk strength, Tauern wind in East Tirol. Subsequently, SW foehn winds. Snow Layering Last night in Tirol there was a small amount of snowfall, brisk W/SW winds whipped up and transported it. The drifts which formed are small, but quite prone to triggering. The intensifying solar radiation, together with nocturnal outgoing radiation, consolidated the snowpack surface on steep, sunny slopes more than anywhere else. However the weak inner layering of the snowpack is still worrisome. Particularly on shady slopes above 2200m, the fundament is riddled with loose, faceted snow crystals. Avalanche Danger Avalanche danger in Tirol’s backcountry touring regions is regionally considerable above 2200m. The major peril stems from fresh, rather small-sized snowdrift accumulations which can often trigger an avalanche even by minimum additional loading. Avalanche prone locations are found in ridgeline terrain in all aspects, in drifted gullies and bowls, and generally in transitions from shallow to deep snow. Particularly in those regions where the snow structure is poor, i.e. inneralpine regions and on the Carnic Ridge, can avalanches fracture down to more deeply embedded layers inside the snowpack and then grow to large size. The situation in the regions where snowfall has been heavy (in the west and north) is more favourable.