for this study. For example, topo-
graphic data at a 500 500 m horizontal resolution are
included and the horizontal discretization is changed from
1 1 km to 500 500 m to better describe the land surface
variations and improve representations of streams. The
unsaturated zone is included as an integrated part of the
model, with the purpose to (1) simulate the interaction
between changes
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
catchments (Crochet, 2013).
This method attempts to predict future streamflow on the basis of the comparison of current
and past streamflow and meteorological observations. This technique has been used in stream-
flow forecasting by, for example, Karlsson & Yakowitz (1987), Galeati (1990) and Akbari et al.
(2011). The advantage of this technique is its simplicity, as there is no need to describe/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
1987).
The dynamical system under study here is the hydrologic response of a watershed to atmo-
spheric forcing and physiography, which is governed by complex processes taking place at
different spatial and temporal scales. Rather than to attempt to explicitly describe these pro-
cesses through hydrological modeling, the analogue method proposed here simply attempts to
predict future streamflow
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf