Abstract
Run-off formation, the spatial processes that lead to water entering the channel network, is described in its representation in DANUBIA. The representation includes direct run-off and interfl ow, which are a product of infi ltration capacity and water movement in the unsaturated soil layers. As a result the exemplary case of the year 1999 as well as a comparison of the simulated run-off formation and measured discharges at selected gauges for the period 1971-2000 is shown.
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Mauser, W., & Ludwig, R. (2016). Run-off formation. In Regional Assessment of Global Change Impacts: The Project GLOWA-Danube (pp. 201–206). Springer International Publishing. https://doi.org/10.1007/978-3-319-16751-0_25
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