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The specific characteristics of catchments disturbed by lignite mining are presented for the Schlabendorf/Seese region, where a close relation between water issues and open-cast lignite mining exists.
Hierarchical cluster, ordination analysis, the Budyko framework, and generalized additive models were used to evaluate hydrological similarity, extract the dominant response, and examine how the landscape and climatic characteristics of catchments influence the dominant streamflow response.
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Hydrological investigation and behavior of watershed depend upon geo-morphometric characteristics of catchment.
Areal aspect represents the characteristics of catchment area and describes how catchment area controls and regulates the hydrological behaviour.
The transit time of water is a fundamental characteristic of catchment functioning and can often be related to water quality dynamics, thus providing potentially important information for water managers in these environments.
The model determines the location of rivers, divides basin to sub basins and extracts physical characteristics of the catchments.
These results can aid in understanding the particular runoff generation characteristics of granitic catchments.
Traditional conceptual models have the disadvantage of requirement of spatial variation parameters about the physical characteristics of the catchments.
Morphometric characteristics of the catchments were computed both from ASTER digital elevation model (DEM) and topographic maps.
This study implicates the necessity of including remotely sensed geomorphologic characteristics of ungauged catchments to improve flood predictions in these regions.
During the later period (1996 – 2006) the trends reversed, i. e., catchment IV recorded the lowest (14. 1 t ha- 1) soil loss whereas catchment I recorded the highest (23. 4 t ha- 1) soil loss despite the fact that there was no change in the status of soil conservation or the characteristics of the catchments.
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