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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 interflow, which are a product of infiltration 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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Correspondence to Wolfram Mauser .

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Mauser, W., Ludwig, R. (2016). Run-Off Formation. In: Mauser, W., Prasch, M. (eds) Regional Assessment of Global Change Impacts. Springer, Cham. https://doi.org/10.1007/978-3-319-16751-0_25

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