Publication: Influence of snowmelt and heavy rainfalls on water and sediment yield from loess gully catchment (Lublin upland – Poland)
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The surface discharge from the gully catchments of the Lublin Upland (Poland) usually is not very high and amounts to about 15 mm·yr-1. It is mainly an episodic discharge of snow/rainfall regime. Surface runoff and rill erosion are caused by rains of the total >10 mm and intensity >1 mm·min.-1, the main factor of gully erosion is however snowmelt runoff. Most of the material set in motion at that time remains at the bottom of the gully, and can be carried away during heavy rainfalls.
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