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Results:

• 11. vanRoosmalen_etal-2009-WRR_2007WR006760

  and evapotranspiration to the surface and groundwater system. The vegetation type deter- mines the transpiration properties through the crop factor and the root depth, and the fraction of precipitation that is intercepted by the canopy. Land use changes can therefore reduce or amplify future climate change induced hydrological impacts in a catchment. [3] A number of studies have focused on the effects /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 12. VI_2014_005

  , Veðurstofu Íslands   Contents 1 Introduction ................................................................................................ 7 2 Model setup and data ................................................................................... 7 3 Model terrain and surface type ...................................................................... 9 4 Impact of initial conditions in blending /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

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

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 14. 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

• 15. Irafossmyndir_1-4

  
  Mynd 1
  Mynd 2 
  Mynd 3
  Mynd 4 /media/geislun/myndasafn/Irafossmyndir_1-4.doc

• 16. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  networks for t i Christiansen Barlebo r Voldgade 10, DK-1350 Copenhagen K, Denmark form 3 May 2007; accepted 11 May 2007 29 June 2007 www.elsevier.com/locate/jenvman  Mak manage ARTICLE IN PRESS brought together to find a solution that is adequate from multiple perspectives. This, not only requires coping with various sources and types of uncertainty, but also with the ambiguity produced /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 17. 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

• 18. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 19. VI_2020_005

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.4.1 Sea level projections for Scandinavia, the UK and Iceland . . . . . . . . . 29 2.5 Extreme sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 2.5.1 Extreme sea levels in Scandinavia, the UK and Iceland . . . . . . . . . . . 36 3 Coastal flooding risk analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40 3.1 Coastal flooding risk /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

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

  part of Upper Tisza. Based on data from EM-DAT: The OFDA/CRED International Disaster Database 2008 1 For a disaster to be entered into the Emergency Events Database (EM-DAT) at least one of the following criteria must be fulfilled: (1) Ten or more people reported killed; (2) Hundred people reported affected; (3) Declaration of a state of emergency; (4) Call for international assistance (From: EM /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf