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Rainfall triggering soil slips in the southern Apuan Alps (Tuscany, Italy)

机译:降雨引发南部阿普安阿尔卑斯山的滑坡(意大利托斯卡纳)

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The Apuan Alps are characterized by frequent heavy rainfall. In severalcases this triggered many shallow landslides (soil slips). With the aim ofcontributing to the landslide hazard evaluation of the southern Apuan Alps(upper Versilian area), a detailed analysis of the main pluviometric eventswas carried out. Data recorded at the main raingauge of the area from 1975to 2002 were analysed and compared with the occurrence of soil slips, inorder to examine the relationship between soil slip initiation and rainfall.Some thresholds for soil slip-debris flow activity in terms of meanintensity, duration and mean annual precipitation (MAP) were defined for thestudy area.
机译:阿普安阿尔卑斯山的特点是经常降雨。在某些情况下,这引发了许多浅层滑坡(泥石流)。为了有助于评估南部阿普安阿尔卑斯山(上西西里地区)的滑坡灾害,对主要的测雨事件进行了详细分析。分析了该地区1975年至2002年主要雨量计记录的数据,并将其与土壤滑坡的发生进行了比较,以便研究土壤滑坡的形成与降雨之间的关系。定义研究区域的年平均降水量(MAP)。

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