Eserved as relict landforms within the southern sector. Land 2021, 10, x FOR PEER Assessment Moreover, various N -oriented avalanche tracks characterize the norther escarpment 12 of 35 from the Corno Piccolo ridge, alternating themselves together with the rock gullies.Figure six. Simplified geomorphological map on the study area (modified and updated from [65,88,89]). The black line Figure six. Simplified geomorphological map in the study area (modified and updated from [65,88,89]). The black line represents the study region. represents the study location.Huge quiescent rotational and translational slides impact the central-eastern portion 4.3. Climatic Evaluation of your study area east with the Prati di Tivo area, with each other with localized quiescent The microclimatic features and study region have been analyzed thinking about the historical earthflows. Smaller rotational of thetranslational slides are discovered towards the north, thermo luviometric series offered at theFinally, N -oriented rockm a.s.l.),with debris primarily set on pelitic-arenaceous deposits. Pietracamela gauge (1043 gullies covering a 50-year time period (1951004); nevertheless,the Corno Piccolo ridge. Landforms resulting from discharges characterize the northern slop of your selected gauge is Deguelin Activator positioned approximately operating water are primarily represented by a wide alluvial fan, at the same time as of quite a few gullies; both are present within the western part of the study location, within the Prati di Tivo location, the former getting set in between glacial (towards the West) and AZD1208 supplier landslide (to the East) deposits, the latter using a basic N path and extending along the key drainage line. Ultimately,Land 2021, 10,13 of400 m beneath the Prati di Tivo region and at least 1000 m downstream on the primary avalanches and landslides detachment places (Table two). Nonetheless, for the study location, it was not possible to define spatial and altitudinal meteoric features considering that snowfall and rainfall events are frequently coupled with sturdy winds which will induce relevant prices of underestimations, in particular in the highest elevations.Table two. Most important values of the temperature and rainfall, resulting in the climatic evaluation in the Pietracamela gauge (1043 m a.s.l.).Yearly Average (1951004) Temperature ( C) Frost days Absolute maximum Day-to-day average Mean maximum Imply minimum Absolute minimum 65 36.8 ten.7 14.6 six.7 Frost days Absolute maximum Daily typical Imply maximum Imply minimum Absolute minimum Jan 16 19 three six.5 Feb 15 20.7 three.4 7.2 Mar 12 25 5.5 9.four 1.five Monthly Average (1951004) Temperature ( C) Apr Could Jun four 24.five 8.4 12.four 4.four 0 31.5 12.8 17 eight.7 0 35 16.7 21.2 12.3Jul 0 35 19.7 24.5 14.9 four.Aug 0 36.8 19.eight 24.six 14.9Sep 0 34 16 20.two 11.Oct 1 27.8 11.three 14.9 7.Nov five 25 7.two ten.4Dec 12 22 4.two 7.4 1.-0.four –0.–12.eight -12.–0.-1.—Rainfall (mm) Total rainfall Maximum in 1 h Maximum in 24 h Rainy days 1065.3 57.eight 268.six 106 Total rainfall Rainy days Jan 85.4 eight.five Feb 74.8 9.1 Mar 95.7 9.7 Apr 110.4 ten.6 May well 82.five 10.0 Jun 68.1 eight.0 Jul 44.9 6.2 Aug 51.eight 5.eight Sep 78.three 7.2 Oct 117.1 9.eight Nov 136.3 ten.8 Dec 120.0 10.The typical annual temperature is 10.7 C, with an typical every day thermal excursion of 7 C; the maximum temperatures can ultimately exceed 35 C, even though the minimum ones pretty much reach -15 C. Frost days (Tmin 0 C) are 65 per year, even though ice days (Tmax 0 C) are no a lot more than ten per year. The total rainfall is moderately abundant with respect for the Gran Sasso Massif geographic place, exposed to “Tramontana” and “Bora” dry and cold winds, also as to “Scirocco” and “Libeccio” wetter ones, which o.
