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Ehret, U. (author), Gupta, H.V. (author), Sivapalan, M. (author), Weijs, S.V. (author), Schymanski, S.J. (author), Blöschl, G. (author), Gelfan, A.N. (author), Harman, C. (author), Kleidon, A. (author), Bogaard, T.A. (author), Wang, D. (author), Wagener, T. (author), Scherer, U. (author), Zehe, E. (author), Bierkens, M.F.P. (author), Di Baldassarre, G. (author), Parajka, J. (author), Van Beek, L.P.H. (author), Van Griensven, A. (author), Westhoff, M.C. (author), Winsemius, H.C. (author)
Throughout its historical development, hydrology as an earth science, but especially as a problem-centred engineering discipline has largely relied (quite successfully) on the assumption of stationarity. This includes assuming time invariance of boundary conditions such as climate, system configurations such as land use, topography and...
journal article 2014
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Krzeminska, D.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Van Beek, L.P.H. (author)
The importance of hydrological processes for landslide activity is generally accepted. However, the relationship between precipitation, hydrological responses and movement is not straightforward. Groundwater recharge is mostly controlled by the hydrological material properties and the structure (e.g., layering, preferential flow paths such as...
journal article 2013
document
Krzeminska, D.M. (author), Bogaard, T.A. (author), Malet, J.P. (author), Van Beek, L.P.H. (author)
The importance of hydrological processes for landslide activity is generally accepted. However, the relationship between precipitation, hydrological responses and movement is not straightforward. Groundwater recharge is mostly controlled by the hydrological material properties and the structure (e.g. layering, preferential flow paths such as...
journal article 2012
document
Krzeminska, D.M. (author), Bogaard, T.A. (author), Van Asch, T.W.J. (author), Van Beek, L.P.H. (author)
Hydrological processes control the behaviour of many unstable slopes, and their importance for landslide activity is generally accepted. The presence of fissures influences the storage capacity of a soil and affects the infiltration processes of rainfall. The effectiveness of the fissure network depends upon fissure size, their spatial...
journal article 2012
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