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Results:

• 11. VI_2015_006

  m 2 or less, compared with losses of 80 W m 2 or more over neigh- bouring cloud-free regions. The conditions around midnight, off the southeast coast on 27 July, and along the north coast on 3 September, clearly show the limited ability (in the model) of even a complete high-level cloud cover to affect the longwave radiation balance at the surface. Mid- level clouds are usually simulated together /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 12. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  & Hautala, R. 2009. Benefits and value of meteorological information services – the case of the Finnish Meteorological Institute, Meteorological Applications, 16, pp. 369–379. Meyer, M.D., Amekudzi, A., O’Har, J.P. (2009), Transportation Asset Management Systems and Climate Change: An Adaptive Systems Management Approach, paper for Transportation Research Board 2010 Annual Meeting, CD-ROM /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 13. Lorenzoni_Pidgeon_2006

  for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 14. Supercomputer in Iceland

  together on climate studies, Arctic studies, development and operation of the Harmonie model and other topics of mutual interest. The cooperation allows for new research opportunities, as well as further development of Nordic and International collaboration. In order to be able to accommodate the supercomputer at IMO's site, the infrastructure had to be upgraded, i.e. the uninterruptible power supply /about-imo/news/nr/3309

• 15. Twenty years of multinational earthquake prediction research in Iceland, and the future

  As in all earthquake-prone countries it has for a long time been a challenge for Icelandic seismologists to be able to warn about large earthquakes. During 1988-2005 Icelanders coordinated four international prediction research projects, with Iceland as a test-area, to build a base for earthquake warnings and better hazard assessments. The SIL project (1988-1995) was a concerted effort /earthquakes-and-volcanism/conferences/jsr-2009/earthquake-prediction/

• 16. Jokull-guidlines

  mm and the distance between lines not less than 0.2 mm. Foldouts can only be accepted in exceptional cases. All illustrations should be identified lightly with a pencil on the back with the name of the author and the figure number. Formulae and algebraic symbols should be indicated clearly. Equations should be numbered sequentially. Numbers in brackets can refer to formulae /media/jar/Jokull-guidlines.pdf

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

  are currently melting at a fast rate. Over recent decades, annual mass balance field observations on the three largest ice caps in Iceland* Langjo¨kull (ca. 900 km2), Hofsjo¨kull (ca. 890 km2) and Vatnajo¨kull (ca. 8100 km2)*show a declining specific mass balance from about 0 m yr1 w. eq. on average from 1980 to 1994 to 1 to 1.3 m yr1 w. eq. on average after 1995 (Bjo¨rnsson et al. 2002 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 18. Isskyrsla_20100119_3

  Ísskýrsla TF-SIF 19. janúar 2010 Flug nr. 00310.025 Áhöfn: Flugstjóri Hafsteinn Heiðarsson Flugmaður Benóný Ásgrímsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Hreggviður Símonarson Stýrimaður Vilhjálmur Óli Valsson Stýrimaður Aðrir Flugleið: Þriðjudaginn 19.janúar 2010 fór flugvél Landhelgisgæslunnar í eftirlits – og ískönnunarflug fyrir /media/hafis/skyrslur_lhg/Isskyrsla_20100119_3.pdf

• 19. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 20. Journal_of_Hydrology_Veijalainen_etal

  the cascade of uncer- tainty becomes greater, which is always the case in this kind of complex analysis of climate change and extreme events (e.g. Men- zel et al., 2006). 3.1. Climate scenarios The climate scenarios in this study are from four global climate models (GCM) and means of 19 global climate models with three SRES (IPCC, 2000) emission scenarios (A2, B1 and A1B) and four re- gional /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf