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• 61. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 62. VI_2013_008

  of letters indicates the origin of flow with the first letter indicating the primary origin. Three of these catchments are partly glaciated and two of them have a large groundwater contribution (vhm 64 and vhm 66). A more detailed de- scription of the hydrology of these catchments can be found in Crochet (2013) where a study of their hydrologic response to recent climate variations is presented /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 63. VI_2014_006

  l l l l 5 10 15 20 − 1. 0 − 0. 8 − 0. 6 − 0. 4 − 0. 2 0. 0 method De g. C el siu s ME T2m − Analysis l vhm10 vhm19 vhm26 vhm64 vhm66 l l l l l l l l l l l l l l l l l l l l 5 10 15 20 2. 0 2. 2 2. 4 2. 6 2. 8 3. 0 method D eg . C el siu s RMSE T2m − Analysis l vhm10 vhm19 vhm26 vhm64 vhm66 Figure 3. Results of intercomparison of twenty different analogue methods. Mean error (left) and RMSE /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf