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Results:

• 21. VI2010-006_web

  5.6 Hafnarstræti 23–89 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 5.7 Grófargil . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36 5.8 Gleráreyrar og farvegur Brunnár . . . . . . . . . . . . . . . . . . . . . . . . . 36 6 Niðurstaða 37 7 Heimildir 38 Viðaukar I Tæknileg hugtök og skilgreiningar 41 II Langsnið brauta 43 III Kort 49 5 6 1 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 22. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigation Current climate 560 23 264 243 10 18 A2 scenario + 74 (13%) 0 + 50 (19%) 0 0 + 16 (89%) B2 scenario + 118 (21%) +1 (4%) + 84 (32%) + 20 (8%) 0 + 9 (50%) aWater balance values are in millimeters. Relative changes are in parentheses. Table 4. Spatially Averaged, Mean Monthly Recharge for the Current Climate and the A2 and B2 Scenarios for the Simulation Without Abstractions /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 23. VI_2020_004

  ) ................. 89 Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90 Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91 Figure 63 Preliminary intersectional map ................................................................................ 93 Figure 65 Initial user-interface of the public web-site /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 24. 2010_003rs

  A (A1, A2, A3). ........................................................................................... 89 Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90 Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90 Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 25. VI_arsskyrsla2020

  /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 26. GA_2009_91A_4_Andreassen

  of –0.03 m w.e.The reason for this increase in sensitivity is thatthe period of ice and firn melt will increase in a warmer climate. As an example, model calcula-tions show that the number of days where the sur-face is ice at the 1575 m a.s.l. altitude (AWS-lo- cation) is 41 days in the reference period 1969–2006. Increasing the temperature by +2°C will re- sult in more than a doubling to 89 days /media/ces/GA_2009_91A_4_Andreassen.pdf

• 27. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 28. Eriksson_Garvill_Nordlund_2006

  (F ð1; 905Þ ¼ 6:89, po0:01, partial Z2 ¼ 0:008), and a larger reduction in own and others’ car use compared to the increase with two SEK/l (F ð1; 880Þ ¼ 16:96, po0:001, partial Z2 ¼ 0:019 and F ð1; 879Þ ¼ 15:64, po0:001, partial Z2 ¼ 0:017 respectively). In addition, the increase with five SEK/liter was perceived as more unfair (F ð1; 904Þ ¼ 10:06, po0:01, partial Z2 ¼ 0:011) and respon- dents /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 29. Kok_et_al._TFSC_published_2011

  /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 30. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf