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that
is required to create a transition towards adaptive management.
3.2 Identification and Characterisation of Uncertainties in the IWRM Process
In the next sections, uncertainties emerging in the IWRM process are characterised by their
nature, type and source according to the above classification. The location of the
uncertainty is described with reference to the key IWRM steps shown in Fig. 2/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
combinations indicate the
type of river, with the first letter indicating the primary type. Direct runoff river (D), presence
of lakes (S), glacier-fed river (J), groundwater (L).
Gauging station vhm vhm vhm vhm vhm vhm
19 10 26 145 66 64
Name Dynjandisá Svartá Sandá Vestari- Hvítá Ölfusá
Jökulsá
Type of river D+L D+L D+L D+J+L L+J L+D+J+S
Drainage area (km 2) 42 397 267 850 1664 5687
Mean altitude (m a.s.l
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf