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Results:

• 11. VI_2014_005

  absolute errors (MAEs) are listed in Table 1. For temperature, the overall bias in January is reduced by 86%, with a reduction in overall MAE of 17%. For wind speed, the overall January bias is reduced by 74%, with a reduction in overall MAE of 9%. Both, for temperature and wind speed, the main benefit of the correction procedure is a reduction of differences between monthly mean values. Mean absolute /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 12. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  Journal of Environmental Management 88 Heid , Øste d e A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a Human dependence on water leaves us vulnerable to climate change, flood and drought hazards, and poverty dynamic element of vulnerable groups and their relation- ship to water resources, and to represent the decisions /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 13. 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

• 14. VI_2020_005

  ) and are Global Navigation Satellite System (GNSS) data providers (SONEL, n.d.). The North Sea is home to one of the most dense tide gauge networks in the world, with over 15 tide gauge series that span at least 100 years along its coastline (Quante and Colijn, 2016). In Denmark, 17 the national tide gauge network consists of 90 automatic stations run in cooperation of the Danish Meteorological /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

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

  of the glaciers. An up to 8 m thick winter snow layer was measured in the accumulation area (∼4 m w.e.). Ice melt of up 10 m w.e. was measured in the lowest part of the ab- lation zone in summer, and 2 m w.e. was melted during win- ter. Taking into account ∼2 m of annual rainfall, the runoff from this part of the glacier was estimated as ∼14 m w.e. per year; a surprisingly high value (Ahlmann, 1939 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 16. 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

• 17. VI_2009_006_tt

  the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average propagation speed of the subglacial jökulhlaup flood front was found to be in the range 0.2–0.4 m s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 18. 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

• 19. 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

• 20. 2010_005_

  in the ENSEMBLES project. . . . . . . . . . . . . . . . . . . . . . . . . 37 16 Mean seasonal cycle during the 1961–90 control period, the 2021–50 reference period, and the 2070–99 reference period, for the IPCC ensemble mean, the SMHI- RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . . . . . 38 17 Changes in the mean seasonal cycle from the 1961–90 control to the 2021–50 refer- ence /media/ces/2010_005_.pdf