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Results:

• 11. CES_D2.4_task2_CMIP3_winds

  changes in the September-April mean geostrophic wind speed from 1971- 2000 to 2046-2065 (left) and the statistical significance of the ensemble mean change according to a standard t test (right). Light, medium and dark red shading indicate significance at the 95%, 99% and 99.9% levels, respectively. 95 % 99 % 99,9 % 4 Fig. 4. As Fig. 3, but for the autumn (September /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 12. VI_2022_006_extreme

  Þingvallavatn 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 12 15 18 19 21 23 6 hours 26 31 35 38 41 44 12 hours 48 56 62 67 73 77 24 hours 78 90 99 107 117 124 48 hours 113 128 138 148 159 168 26 Figure 12 – 1M5 map for catchment Hálslón based on the complete ICRA dataset. Figure 13 – 1M5 map for catchment Þingvallavatn based on the complete ICRA dataset. 27 5.2 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 13. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  (on CC impact s and )i s use d in publi c debate s (an di s no t distorted ) Raadgeve re t al .( 200 8) Ne w informatio n (on CC impacts )influence s polic y 24 .Decisio n suppor t syste m Rive rbasi n informatio n system s ar e u p to internationall y recognize d standard s (e.g .WB/UND P standards ) Youn g (200 2), Willi s an d Whittake r( 200 2) Climate change adaptation in European river basins /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 14. CES_D2_2_poster_3x3

  /media/ces/CES_D2_2_poster_3x3.pdf

• 15. CES_D2.4_task1

  MIETOINEN SAARI FI +60:37:48 +21:52:12 13 T 706 TURKU AIRPORT FI +60:30:00 +22:16:12 47 TP 708 JOKIOINEN OBSERVATOR FI +60:49:12 +23:30:00 104 T 710 UTTI AIRPORT/VALKEAL FI +60:54:00 +26:55:48 99 T 717 KAUHAVA AIRPORT FI +63:06:00 +23:01:48 42 T 718 AHTARI MYLLYMAKI FI +62:31:48 +24:13:12 157 /media/ces/CES_D2.4_task1.pdf

• 16. VI_Arsskyrsla_2018_vef

  by the inhabitants on a daily basis for driving between towns and villages for work, school, hobbies or di?erent services. Public avalanche bulletins are also published for selected areas, aimed towards the increasing number of backcountry travellers in Iceland during winter time. The number of human-triggered avalanches recorded by the Meteorological O>ce has increased substantially over /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 17. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 18. CES_D2.4_VMGO

  /media/ces/CES_D2.4_VMGO.pdf

• 19. Protective measures

  experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html) Stálgrindur eða snjóflóðanet? Val á tegund /avalanches/imo/protective/

• 20. GA_2009_91A_4_Andreassen

  with precipitation data from Fokstua asinput and a much lower correlation (r2=0.48) wasobtained (De Woul and Hock 2005; Table 2) thanthe r2 of 0.75 we obtained by using a combinationof Bulken and Røldal. Their observation period was shorter (45 years) than the period used in thisstudy (58 years). Rasmussen and Conway (2005)obtained r2=0.63 using an upper-air model for theperiod 1948/49–1998/99 /media/ces/GA_2009_91A_4_Andreassen.pdf