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The study presents the geomorphological effects of extreme hydroclimatic phenomena such as violent downpours, widespread rainfalls with a high sum of precipitation, and intensive snowmelt occurring in the eastern part of Polish Uplands between the Vistula and the Bug rivers. The intensity and impact of these phenomena on relief is exceptionally varied here due to the variety of natural conditions...
On the 31st July – 6th August 2005 in Lublin surroundings, high and intensive rainfalls appeared (Table 1). The highest one took place at night of 3rd–4th August and its level exceeded 100 mm in two stations (Fig. 1). It was the rain of changeable intensity to 1 mm·min–1, lasting 4–5 hours. In the area of 400 square kilometers enclosed with 100 mm isohyet, an intensive runoff with erosional effects...
Rozwój procesów erozyjnych na lessowej skarpie uprawowej koło Garbowa na Wyżynie Lubelskiej obserwowano w obfitujących w opady ulewne latach 1995-2001. Badana skarpa powstała przy dnie doliny nieckowatej w miejscu, gdzie biegnąca prawie równolegle do jej osi miedza, podcina garb na zboczu. Analiza profilu glebowego dowodzi, że utworzenie skarpy spowodowała głównie erozja pod miedzą, uwarunkowana jej...
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