drought-supporting
WTs over previous n days (n = 1, 15, 30, 45, 60, 90, 120, ... 330).
Determination of the period of influence: dreg
90
45 little groundwater45
45
CES conference, Oslo, Norway, 31 May - 2 June 2010
210
60
45
60
highly productive
aquifers
moderately
productive
aquifers}90
210
60
60
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe
/media/ces/AnneFleig_May2010_CES.pdf
boundary flux between the unsaturated zone and the groundwater (Schulla
& Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each watershed by comparison of modelled and
measured discharge series.
In this study
/media/ces/2010_017.pdf
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Ensemble approach for probabilistic
hydrological projections
Catchment
/media/ces/Lawrence_Deborah_CES_2010.pdf