Ing and analysis in diverse geological and climatic contexts, as field-based and numerical analysis [937]. effectively as field-based and numerical analysis [937].3.3. Climatic Analysis 3.3. Climatic Analysis Climatic information analysis was carried out to outline the distribution from the climatic Climatic data evaluation was carried out to outline the distribution from the climatic parameters and situations inside the study area. The evaluation was based on a dataset obtained parameters and situations in the study region. The analysis was based on a dataset obtained from a network of 7 gauges (colored dots in Figure 4; data supplied by the Functional from a network of 7 gauges (colored dots in Figure four; data offered by the Functional Center and Hydrographic Workplace with the Abruzzo Region and the amateur meteorological association L’Aquila Caput Frigoris–caputfrigoris.it/, accessed on 12 January 2021). A lot more in detail, in line with the lack of historical thermo luviometric series suiting the Planet Meteorological Organization (WMO) directives [98], climatic information belonging to the Pietracamela gauge (1043 m a.s.l.; blue dot in Figure 4) had been made use of to quantify the microclimatic setting from the study location properly. Its dataset gathers thermo luviometricLand 2021, ten,eight ofseries data covering a 50-year time record (1950004). Lately, 3 gauges, featuring technical elements in accordance with all the WMO 1083 directives [98], were located at the Teramo (265 m a.s.l.; pink dot in Figure four), near the tourist and ski facilities at Prati di Tivo (1450 m a.s.l.; green dot in Figure 4), and along the northeastern slope of Gran Sasso Massif at Rifugio Franchetti (2433 m a.s.l.; light blue dot in Figure 4). The northern exposure of those gauges gives an excellent representation of your climatic conditions occurring in correspondence with the detachment places of snow avalanches, regardless of the lack within the snow datasets. Regarding the Rifugio Franchetti gauge, the obtainable data covered JR-AB2-011 web unique time records (1998003 and 2016018). three.4. Nivological Evaluation The nearby nivological analysis was primarily based on a detailed dataset manually collected at the nivo-meteorological station of the Meteomont service (sian.it/infoMeteo, accessed on 15 February 2021). It truly is located in the base from the slope in the Prati di Tivo location (Figure 3), at an elevation of 1450 m a.s.l. It characteristics a northern exposure comparable to avalanche-prone regions positioned at larger elevations. The available historical information for this station begins in the 1977/1978 winter season (from November to April) for 32 surveying seasons. The series is practically uninterrupted, with a couple of gaps mainly occurring in correspondence of the AZD1208 custom synthesis beginning/end of seasons. Having said that, data associated towards the 1992/1994 seasons are absolutely missing. Extra in detail, the regarded dataset shows quite a few temporal gaps, since it’s deeply affected by the irregularity within the opening/closing dates of ski facilities–the former occurring immediately after the initial important snowfall events plus the latter throughout the spring period, typically within the presence of a thick snow cover. This condition was extensively relevant prior to the 1986/1987 winter season and immediately after the 2008/2009 one particular; consequently, the amounts of seasonal new snow weren’t appropriately computed in these temporal intervals. To decrease this underestimation, we tried to derive good-quality data about the prospective snowfall events by computing thermo luviometric records at gauges positioned at a comparable elevation not far from the Pr.
