Debris flow at the Kirilova poliana (Rila Mountain) on August 22, 2022

A. Sarafov, S. Matev, Dimitar Krenchev, G. Rachev
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Abstract

In the present study is characterized the synoptic situation and conditions, which led to a debris flow event in the Manastirska River valley on August 22, 2022. The main reason for the occurrence of this hazardous events is predetermined by one of the right tributaries of the Manastirska River. For the purpose of the study, several morphometric parameters of the tributary were calculated and analyzed such as area and shape of the basin, slopes, aspect, drainage network length, drainage density, etc. The type and the transportation of the sediments were determined by measurements, grain-size and clast-shape analysis. The impact of weather conditions on debris flow occurrence were determined by the analysis of the synoptic conditions on the days before the event.
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2022年8月22日,Kirilova poliana(里拉山)的泥石流
本文对2022年8月22日马纳斯提尔斯卡河流域发生泥石流事件的天气条件进行了分析。发生这种危险事件的主要原因是由马纳斯提尔斯卡河的右边支流之一预先决定的。为此,计算并分析了流域面积和形状、坡度、坡向、水系网长度、水系密度等支流形态计量参数。通过测量、粒度和碎屑形状分析确定了沉积物的类型和搬运。天气条件对泥石流发生的影响是通过分析泥石流发生前几天的天气条件来确定的。
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