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Results:

• 1. Water_resources_man_Veijalainen_etal

  Echam5-A2 4.34 18.7 5 ECHAM5/MPI-OM – A1B Echam5-A1B 4.13 17.2 6 ECHAM5/MPI-OM – B1 Echam5-B1 3.17 12.9 7 UKMO-HadCM3 – A2 HadCM3-A2 5.16 11.4 8 UKMO-HadCM3 – A1B HadCM3-A1B 5.21 15.7 9 UKMO-HadCM3 – B1 HadCM3-B1 3.73 18.3 10 CCSM3 – A2 CCSM3-A2 4.77 15.1 11 CCSM3 – A1B CCSM3-A1B 3.56 12.5 12 CCSM3 – B1 CCSM3-B1 2.70 7.0 13 UKMO-HadCM3 RCA3 A1B RCA3-H-A1B 4.44 33.8 14 ECHAM5/MPI-OM RCA3 A1B RCA3-E-A1B /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 2. 2013_001_Nawri_et_al

  Office Halldór Björnsson, Icelandic Met Office Kristján Jónasson, University of Iceland 4 Contents 1 Introduction 9 2 Spatial and temporal variability of low-level wind 11 3 Methodology 13 3.1 Wind modelling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Weibull statistics . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 3.3 Density /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 3. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  subglacial eruption in the Eyjafjallajo¨kull volcano. Iceland is located in the North Atlantic Ocean (Fig. 1), at the confluence of air/water masses from the mid- latitudes and from the Arctic. About 11% of Iceland is covered by glaciers, all of which are temperate, have a high annual mass turnover and are highly sensitive to climate fluctuations (e.g., Bjo¨rnsson 1979; Bjo¨rnsson & Pa´lsson 2008 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 4. Paper-Olafur-Rognvaldsson_91

  –3012. Warner, T. T., Peterson R. A. and Treadon R. E. 1997. A tutorial on lateral boundary conditions as a basic and potentially serious limitation to regional numerical weather prediction. Bull. Amer. Meteorol. Soc., 78(11), 2599–2617. /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 5. Bardarbunga_kafli20140825

  volcanic system has been highly active in the Holocene with at least 26 eruptions in the last 11 centuries. The last eruption took place in 1910 CE. The Bárðarbunga system lies on the Eastern Volcanic Zone and is about 190 km long and up to 25 km wide, consisting of a central volcano rising to 2009 m a.s.l. and a fissure swarm partly covered by the Vatnajökull ice cap. The central volcano has /media/jar/Bardarbunga_kafli20140825.pdf

• 6. VI_2017_009

  .................................................................................................................... 10 3 Which domain, resolution, and models of the CORDEX project should be selected for the analysis of 21st century climate change in Iceland? .............................................. 11 3.1 EURO domain versus Arctic domain ................................................................. 11 3.2 EURO-44 domain versus EURO-11 domain /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 7. Observations - Ingólfsfjall

  Observations - Ingólfsfjall | Observations | Icelandic Meteorological office Observations - Ingólfsfjall Mon 1.05 14 GMT 5.6° E 3 Max wind : 5 / 7 13 GMT 5.4° ENE 5 Max wind : 7 / 9 12 GMT 4.3° ENE 8 Max wind : 9 / 13 11 GMT 3.5° ENE 9 Max wind : 10 / 13 10 GMT 2.2° ENE 10 Max wind : 11 /m/observations/areas

• 8. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 9. Veðurstöðvar

  ) O F M I Bræðratunguvegur (sj) O I Búlandshöfði (sj) O I Búrfell (sj) O F M I Dalatangi (sk) O I Dalatangi (sj) I Dettifoss (sj) O I Dreki (xf) I Dyngjujökull (sj) I Egilsstaðaflugvöllur (sm) O F M I Eldhraun (sj) I Ennisháls (sj) O F M I Eskifjörður (sj) O F M I Eyjabakkar (sj) O F M I Eyrarbakki (sj) O F M I Fagridalur (sj) O F M I Fagurhólsmýri (sj) O I Fáskrúðsfjörður Ljósaland (sj) O I /weather/stations/

• 10. Journal_of_Hydrology_Veijalainen_etal

  is the modified daily temperature, Tobs is the observed daily temperature in the reference period, DT is the temperature change, sm is the monthly scaling factor that scales the monthly changes to correspond to the monthly changes of the climate sce- nario and as and bs are the coefficients of the seasonal linear trans- fer functions estimated from daily temperatures of the RCMs. 3.3. Hydrological modelling /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf