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The study on bedload transport was conducted on the gravel-bed Scott River catchment with a glacial alimentation regime, located in the NW part of the Wedel Jarlsberg Land (Spitsbergen) with subpolar climatic conditions. In the melt season of 2010, bedload transport rate was continuously monitored at 24-hour intervals by means of four River Bedload Trap devices aligned across the width of the channel...
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...
W dniach 31 lipca-6 sierpnia 2005 w okolicy Lublina wystąpiły wysokie, intensywne opady (tab. 1). Największy z nich miał miejsce w nocy z 3/4 sierpnia - w dwu stacjach jego wysokość przekroczyła 100 mm (ryc. 1). Był to opad o zmiennym natężeniu do 1 mm/min., trwający 4-5 godzin. W obszarze ok. 400 km2, objętym izohieta 100 mm, wystąpił intensywny spływ powierzchniowy, o skutkach erozyjnych. Wielkość...
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...
On the 15 June 2000 A.D . in the area of the Roztocze Tomaszowskie episodic overland flow from agriculture loess catchment (of 50 ha in area and denivelations up to 50 m ) was observed after 10-minutes of a heavy rainfall (Figure 1 and 2). Twenty water samples were taken to measure the suspension value and the measurement of discharge was made in three streams from the subcatchments of differentiated...
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