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Results:

• 51. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 52. Milly_etal-2008-Stationarity-dead-Science

  water infra- structure projects begun now are large enough to push hydroclimate beyond the range of historical behaviors (19). Some regions have little infrastructure to buffer the impacts of change. Stationarity cannot be revived. Even with aggressive mitigation, continued warming is very likely, given the residence time of atmospheric CO2 and the thermal inertia of the Earth system (4, 20 /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 53. ces_SA_group_flyer_new

  - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % -40 -20 0 20 4 0 6 0 W SP SUM A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % Differences in average Q /media/ces/ces_SA_group_flyer_new.pdf

• 54. Glacial outburst floods

  /volcanoes/volcanic-hazards/glacial-outburst/

• 55. GA_2009_91A_4_Andreassen

  andEnergy Directorate (NVE), Oslo, Norway2Department of Geosciences, University of Oslo, Norway3Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands Andreassen, L. and Oerlemans, J., 2009: Modelling long-term summer and winter balances and the climate sensitivity of Stor-breen, Norway. Geogr. Ann. 91 A (4): 233–251. ABSTRACT. Measurements of winter balance (bw /media/ces/GA_2009_91A_4_Andreassen.pdf

• 56. Refsgaard_etal-2007-Uncertainty-EMS

  BIOMATH, Ghent University, Gent, Belgium d Water Quality Modelling modelEAU, University Laval, Quebec, Canada Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007 Available online 27 April 2007 Abstract A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader water /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 57. Veðurstöðvar

  /weather/stations/

• 58. NONAM_1st_workshop_summary_v3

   peer review  separate from stakeholders Technical input from own  experts and stakeholders  Review of principal options Possible support measures Acceptability & Trade‐offs Deliberation with and  possible mandate from  stakeholders Process & Actions by Core Team    Actor / Source      Policy cycle(s)  Incl. learning  Le ar ni ng fr om e ar lie r c yc le s an d fe ed ba ck fr om o pe ra tio ns /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 59. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ). NeWater is based on the hypothesis that IWRM cannot be realised unless current management regimes undergo a transition towards more 0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvman.2007.05.009 Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50. E-mail address: hjh@geus.dk (H.J. Henriksen). (Downing et al., 2005). Vulnerability /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 60. VI_2009_006_tt

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 3.4 Cumulative volume of floodwater from the Skaftá cauldrons. . . . . . 16 3.5 Discharge in the 2006 and 2008 jökulhlaups from the Western Skaftá cauldron. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 3.6 A transect of the subglacial path of jökulhlaups from the Eastern Skaftá cauldron and the glacier surface. . . . . . . . . . . . . . . . . . . . . 20 3.7 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf