Effects of land use changes on streamflow generation in the Rhine basin (2009)
Terink, W., Uijlenhoet, R., Moors, E.J., Troch, P.A., Verburg, P.H.
The hydrological regime of the Rhine basin is expected to shift from a combined snowmelt-rainfall regime to a more rainfall-dominated regime because of climate change, leading to more extreme flood...
S. W. Lyon, G. Destouni, R. Giesler, C. Humborg, M. Mörth, J. Seibert, ...
Permafrost thawing is likely to change the flow pathways taken by water as it moves through arctic and sub-arctic landscapes. The location and distribution of these pathways directly influence the...
S. W. Lyon, G. Destouni, R. Giesler, C. Humborg, M. Mörth, J. Seibert, ...
Permafrost thawing is likely to change the flow pathways taken by water as it moves through arctic and sub-arctic landscapes. The location and distribution of these pathways directly influence the...
Water Cycle: Modelling and Data Assimilation Across (2008)
H. Leijnse, P. A. Troch, J. Sheffield, W. Castaings, F. X. Ledimet, ...
Adjoint sensitivity analysis and variational data assimilation for flash flood forecasting
Water balance versus land surface model in the simulation of Rhine river discharges (2008)
Accurate streamflow simulations in large river basins are crucial to predict timing and magnitude of floods and droughts and to assess the hydrological impacts of climate change. Water balance models...
Talebi, A., Uijlenhoet, R., Troch, P.A.
Recently, D'Odorico and Fagherazzi (2003) proposed "A probabilistic model of rainfall-triggered shallow landslides in hollows" (Water Resour. Res., 39, 2003). Their model describes the long-term...
Evaluating catchment-scale hydrological modeling by means of terrestrial gravity observations (2008)
Hasan, S., Troch, P.A., Bogaart, P.W., Kroner, C.
In a previous study (Hasan et al., 2006) we applied time series analysis and distributed hydrological modeling techniques to investigate the effect of hydrological processes on observed terrestrial...
Talebi, A., Uijlenhoet, R., Troch, P.A.
Hillslopes have complex three-dimensional shapes that are characterized by their plan shape, profile curvature of surface and bedrock, and soil depth. To investigate the stability of complex...
A steady-state analytical hillslope stability model (2008)
Talebi, A., Troch, P.A., Uijlenhoet, R.
This paper presents a steady-state analytical hillslope stability model to study the role of topography on rain-induced shallow landslides. We combine a bivariate continuous function of the...
A. Talebi, R. Uijlenhoet, P. A. Troch
Recently, D'Odorico and Fagherazzi (2003) proposed "A probabilistic model of rainfall-triggered shallow landslides in hollows" (Water Resour. Res., 39, 2003). Their model describes the...
Climate variability effects on spatial soil moisture dynamics (2007)
Teuling, A.J., Hupet, F., Uijlenhoet, R., Troch, P.A.
We investigate the role of interannual climate variability on spatial soil moisture variability dynamics for a field site in Louvain-la-Neuve, Belgium. Observations were made during 3 years under...
Soil moisture storage and hillslope stability (2007)
Talebi, A., Uijlenhoet, R., Troch, P.A.
Recently, we presented a steady-state analytical hillslope stability model to study rain-induced shallow landslides. This model is based on kinematic wave dynamics of saturated subsurface storage and...
Dry-end surface soil moisture variability during NAFE'06 (2007)
Teuling, A.J., Uijlenhoet, R., Merlin, O., Panciera, R., Walker, J.P., ...
Characterization of the space-time variability of soil moisture is important for land surface and climate studies. Here we develop an analytical model to investigate how, at the dry-end of the soil...
New datasets to estimate terrestrial water storage change (2007)
Troch, P.A., Durcik, M., Seneviratne, S., Hirschi, M., Teuling, A.J., ...
The total amount of water stored in a river basin affects streamflow at various timescales and defines the river basin's response to atmospheric forcing. For example, spring runoff in mountainous...
A steady-state analytical slope stability model for complex hillslopes (2007)
Talebi, A., Troch, P.A., Uijlenhoet, R.
This paper presents a steady-state analytical hillslope stability model to study the role of topography on rain-induced shallow landslides. We combine a bivariate continuous function of the...
Soil moisture storage and hillslope stability (2007)
Talebi, A., Uijlenhoet, R., Troch, P. A.
Recently, we presented a steady-state analytical hillslope stability model to study rain-induced shallow landslides. This model is based on kinematic wave dynamics of saturated subsurface storage and...
Soil moisture storage and hillslope stability (2007)
Talebi, A., Uijlenhoet, R., Troch, P. A.
Recently, we presented a steady-state analytical hillslope stability model to study rain-induced shallow landslides. This model is based on kinematic wave dynamics of saturated subsurface storage and...
Soil moisture storage and hillslope stability (2007)
A. Talebi, R. Uijlenhoet, P. A. Troch
Recently, we presented a steady-state analytical hillslope stability model to study rain-induced shallow landslides. This model is based on kinematic wave dynamics of saturated subsurface storage and...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Estimating spatial mean root-zone soil moisture from point-scale observations (2006)
Teuling, A. J., Uijlenhoet, R., Hupet, F., Van Loon, E. E., Troch, P. A.
Root zone soil moisture is a key variable in many land surface hydrology models. Often, however, there is a mismatch in the spatial scales at which models simulate soil moisture and at which soil...
Estimating spatial mean root-zone soil moisture from point-scale observations (2006)
Teuling, A. J., Uijlenhoet, R., Hupet, F., Van Loon, E. E., Troch, P. A.
Root zone soil moisture is a key variable in many land surface hydrology models. Often, however, there is a mismatch in the spatial scales at which models simulate soil moisture and at which soil...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Estimating spatial mean root-zone soil moisture from point-scale observations (2006)
Teuling, A. J., Uijlenhoet, R., Hupet, F., Van Loon, E. E., Troch, P. A.
Root zone soil moisture is a key variable in many land surface hydrology models. Often, however, there is a mismatch in the spatial scales at which models simulate soil moisture and at which soil...
Estimating spatial mean root-zone soil moisture from point-scale observations (2006)
Teuling, A. J., Uijlenhoet, R., Hupet, F., Van Loon, E. E., Troch, P. A.
Root zone soil moisture is a key variable in many land surface hydrology models. Often, however, there is a mismatch in the spatial scales at which models simulate soil moisture and at which soil...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Topographic convergence and divergence are first order controls on the hillslope and catchment hydrological response, as evidenced by similarity parameter analyses. Hydrological models often do not...
Estimating spatial mean root-zone soil moisture from point-scale observations (2006)
A. J. Teuling, R. Uijlenhoet, F. Hupet, P. A. Troch
Root zone soil moisture is a key variable in many land surface hydrology models. Often, however, there is a mismatch in the spatial scales at which models simulate soil moisture and at which soil...
Assimilation of remotely sensed latent heat flux in a distributed hydrological model (2003)
Schuurmans, J.M., Troch, P.A., Veldhuizen, A.A., Bastiaanssen, W.G.M., Bierkens, M.F.P.
This paper addresses the question of whether remotely sensed latent heat flux estimates over a catchment can be used to improve distributed hydrological model water balance computations by the...
N. Montaldo, V. Toninelli, J. D. Albertson, M. Mancini, P. A. Troch
Recent developments have made land-surface models (LSMs) more complex through the inclusion of more processes and controlling variables, increasing numbers of parameters and uncertainty in their...
Montaldo, N., Toninelli, V., Albertson, J. D., Mancini, M., Troch, P. A.
Recent developments have made land-surface models (LSMs) more complex through the inclusion of more processes and controlling variables, increasing numbers of parameters and uncertainty in their...
Montaldo, N., Toninelli, V., Albertson, J. D., Mancini, M., Troch, P. A.
Recent developments have made land-surface models (LSMs) more complex through the inclusion of more processes and controlling variables, increasing numbers of parameters and uncertainty in their...
Discharge, water table depth, and soil moisture content have been observed at a high spatial and temporal resolution in a 44 ha catchment in Costa Rica over a period of 5 months. On the basis of the...
Analytical solutions to a hillslope-storage kinematic wave equation for subsurface flow (2002)
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subsurface flow from a one-dimensional hillslope with a sloping aquifer can be described by the...
Verhoest, N.E.C., Pauwels, V.R.N., Troch, P.A.
This paper presents two analytical solutions of the linearized Boussinesq equation for an inclined aquifer, drained by ditches, subjected to a constant recharge rate. These solutions are based on...
Assimilation of active microwave observation data for soil moisture profile estimation (2000)
This paper discusses the potential of retrieving information about the soil moisture profile from measurements of the surface soil moisture content through active microwave observations of the Earth....
Streamwater nitrate (NO-3) concentrations along the main stream and at the outlet of several subcatchments within the 114\3 km2 Zwalm watershed in Flanders, Belgium, have been monitored regularly...
Towards the upscaling of local surface flux models. (1996)
Debruyckere, L. F. A., Franks, S. W., Beven, Keith J., Troch, P. A., De Troch, F. P.
Estimation of regional latent and sensible heat fluxes requires the upscaling of local models. One approach is to develop soil-vegetation-atmosphere transfer (SVAT) schemes at different scales...