Ld presents a unimodal distribution, with the maximum values detected in (Figure 8b)surveys, too as from the avalanche inventory and literature information (i.e., Meteomont service), it outcomes that, in correspondence with a sudden temperature rise, January and February. Arguably, for altitudes higher than 2000 m a.s.l., the trend avalanche events may perhaps occur with loose surface cohesion values currently in the 246 h tends to grow to be relatively frequent if not ML372 Modulator bimodal having a second peak in the course of the spring, following the snowfall events, involving many buildings and anthropic structures offered the notable snowfall boost in March and April, as detected in the Campo present within the Prati di Tivo area. Imperatore gauge (2137 m a.s.l.).Figure 9. Seasonal fresh snow trend for the timespan 1986009 (a) and snowfall regime (b) at the Prati di Tivo gauge Figure 9. Seasonal fresh snow trend for the timespan 1986009 (a) and snowfall regime (b) at the Prati di Tivo gauge (1450 m a.s.l.). (1450 m a.s.l.).The number of snowy days shows considerable intra-seasonal variations, strictly dependent on the synoptic seasonal evolution. This aspect was specifically evident inside the last decade, albeit within a context of important snowiness, with values rangingLand 2021, ten,18 ofIn order to provide a total and updated description in the nivometric trends, the historical series and datasets accessible in the Rifugio Il Ceppo gauge (1340 m a.s.l.) have been analyzed. This climate station was taken into account considering that it shows snowmaking very Land 2021, 10, x FOR PEER Assessment similar to that of Prati di Tivo, even if it truly is situated on the eastern side in the neighboring 19 of 35 Laga Mountains at a distance of about 20 km in the study location.Figure 10. Everyday snowfall (a) and snow cover thickness (b) in the Prati di Tivo gauge (1450 m a.s.l.). Figure 10. Day-to-day snowfall (a) and snow cover thickness (b) at the Prati di Tivo gauge (1450 m a.s.l.).So as to provide a full and 11, the nivometric trend spanning over a 40-year As graphically reported in Figure updated description from the nivometric trends, the historical series and datasets accessible boost of snowCeppo gauge (1340 m a.s.l.)is less time period (1979019) confirms the in the Rifugio Il precipitation. Nonetheless, it had been analyzed. This climate station was taken into account considering that using a minimal difference in marked than that evident for the Prati di Tivo region (Figure 8a), it shows snowmaking quite equivalent to that of Prati di Tivo, even ifcmis CNQX Protocol positioned on the eastern side of the neighboring the current interseasonal variations (two.1 it vs. 3.1 cm/season), whose trends are increasingly Laga Mountains at a distance of about 20 km in the study location. marked. As graphically reported in Figure 11, the nivometric trend spanning over a 40-year time period (1979019) confirms the raise of snow precipitation. Nonetheless, it really is much less marked than that evident for the Prati di Tivo area (Figure 8a), having a minimal difference in the recent interseasonal variations (two.1 cm vs. 3.1 cm/season), whose trends are increasingly marked.Land 2021, 10, 1176 Land 2021, ten, x FOR PEER REVIEW19 of 33 20 ofFigure 11. Seasonal fresh snow at Rifugio Il Ceppo (1340 m a.s.l.). The blue dashed line represents the 5-year moving Figure 11. Seasonal fresh snow at Rifugio Il Ceppo (1340 m a.s.l.). The blue dashed line represents the 5-year moving average. average.4.five. Snow Avalanche Hazard Assessment 4.five. Snow Avalanche Hazard Assessment A stepwise methodological ap.