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Results:

• 11. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 12. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  (Rijsberman, 2006). Indicators which acknowl- hypothesis exists that IWRM cannot be realised unless current management regimes undergo a transition toward adaptive management Reflections on the use of Bayesia adaptive managemen Hans Jørgen Henriksen, Geological Survey of Denmark and Greenland (GEUS) Received 19 November 2005; received in revise Available onlin Abstract (2008) 1025–1036 n belief /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 13. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 14. VI_2020_005

  exist that reach back to early 19th century but most series are much shorter (Hamlington and Thompson, 2016). In contrast, satellite altimetry has only been available since the early 1990’s. Satellite altimetry mea- sures the sea surface height, namely the sea level compared to a fixed reference frame (the center of the earth, the geoid or a reference ellipsoid) for latitudes up to 66 N and S (ESA /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 15. 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

• 16. Adalgeirsdottir-etal-tc-5-961-2011

  the location of the mass balance stakes at Breiðamerkurjökull (Bre). The red box indicates the posi- tion of the frame to the right. (C) Hoffellsjökull surface topography in 2001. The ice divide and the model domain are indicated with the red curve enclosing a glaciated area of ∼212 km2 in 2001. Black triangles show the locations of automatic weather stations on the glacier. N is the location /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 17. Reykholt-abstracts

  H. Haraldsson and Tómas Jóhannesson .............................................................................. 29 The mass balance of Brúarjökull, outlet of N-Vatnajökull Ice cap Iceland, in the 20th and 21st century Chris Polashenski ................................................................................................................... 30 Applications of terrestrial lidar /media/vatnafar/joklar/Reykholt-abstracts.pdf

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

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 19. VI_2015_006

  energy. The average net downward shortwave radiation flux at the Earth’s surface during July – August 2008 was found to be 122 W m 2. With a sun altitude angle of 28.86 degrees at solar noon on 1 Au- gust 2008, the net shortwave radiation flux, rescaled to the central latitude of Iceland (65 N), is given by 178 W m 2, and is therefore within the range of overcast and clear-sky values over the snow /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 20. Hare-2011-ParticipatoryModelling

  support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf