Note
Volcanic eruption is ongoing on the Sundhnúksgígaröð crater row. Gas pollution hazard in the area. More

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31. Paper-Olafur-Rognvaldsson_92

a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
32. Refsgaard_etal-2007-Uncertainty-EMS

and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
33. VI_2020_008

/media/vedurstofan-utgafa-2020/VI_2020_008.pdf
34. ces-glacier-scaling-memo2009-01

in Norway was provided by the Norwegian Water Resources and Energy Directorate (NVE). TóJ 12 5.12.2009 Memo References Bahr, D. B., M. F. Meier and S. D. Peckham. 1997. The physical basis of glacier volume–area scaling. J. Geophys. Res., 102(B9), 20,355–20,362. Björnsson, H., and F. Pálsson. 2008. Icelandic glaciers. Jökull, 58, 365–386. Fenger, J. (Ed.). 2007. Impacts of Climate Change on Renewable /media/ces/ces-glacier-scaling-memo2009-01.pdf
35. VI_2014_005

in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
36. BIKF_windrose_2005-2014

45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 33 2 55 2 79 5 88 3 64 2 42 2 49 4 59 5 52 5 38 3 42 1 40 4 41 0 55 3 63 5 55 6 47 5 39 3 34 6 31 3 33 9 33 9 36 6 48 8 53 9 52 6 47 5 33 6 22 3 19 0 16 4 13 0 9 6 11 6 12 0 15 4 Wind rose BIKF April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIKF_windrose_2005-2014.pdf
37. BIVM_windrose_2005-2014

N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 114 8 128 7 84 9 36 1 26 0 13 9 24 3 65 4 136 4 250 3 366 4 298 8 189 6 146 9 99 9 160 6 111 5 83 5 86 1 86 4 80 0 82 6 92 4 96 3 97 5 124 9 109 5 127 7 122 4 115 3 88 0 61 9 52 3 55 3 96 0 109 9 Wind rose BIVM January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 /media/vedur/BIVM_windrose_2005-2014.pdf
38. Gudmundsson-etal-2011-PR-7282-26519-1-PB

Icelandic glaciers. Jo¨kull 58, 365386. Bjo¨rnsson H., Pa´lsson F. & Haraldsson H.H. 2002. Mass balance of Vatnajo¨kull (19912001) and Langjo¨kull (19962001), Iceland. Jo¨kull 51, 7578. Bouillon A., Bernard M., Gigord P., Orsoni A., Rudowski V. & Baudoin A. 2006. SPOT 5 HRS geometry performance: using block adjustments as a key issue to improve quality of DEM generation. ISPRS Journal /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
39. VI_2020_005

/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
40. VI_2009_012

/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf