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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.
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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.
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 recession limb of a hydrograph is the result of the gradual release of water from the catchment which influenced more by the storage characteristics of the catchment.
This study constructs a database of 194 catchments where DOC export was predicted as a function of soil, land-use and hydrological characteristics of each catchment.
The large variation in runoff response can be attributed to the distribution of the rainfall (long-term average 400 mm) and the characteristics of the catchment areas.
Furthermore, depending on the characteristics of a catchment area, the limitation to time of floods can vary.
Therefore, it is necessary to quantify the changes in the run-off characteristics of a catchment under the influence of changed landuse/land cover.
In addition, the model parameters are connected to the physiographical characteristics of the catchment area and are not dependent on the division into sub-basins [28].
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