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Results:

• 11. Bardarbunga-2015_February_events

  was M1.6 today at 08:24. Additionally, five earthquakes were measured around Askja and about 10 around Herðubreið. 19 February 2015 - on pulses and the time lapse between them Earthquake pulses on the caldera rim of 30-90 minutes duration, like the one observed last night, have been characteristic for the seismic activity linked to the caldera subsidence since the beginning of the sequence /media/jar/Bardarbunga-2015_February_events.pdf

• 12. VED_AnnualReport-2013_screen

  (). The circulation of Icelandic waters-a modelling study. Ocean Science , –. Nygaard, B. E. K., Hálfdán Ágústsson & K. Somfalvi-Toth (). Modeling wet snow ac- cretion on power lines: improvements to previ- ous methods using  years of observations. Journal of Applied Meteorology and Climatology (), –. Philippe Crochet (). Sensitivity of Icelandic river basins to recent /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 13. 2005EO260001

  -00046). References Björnsson, H. (2002), Subglacial lakes and jökul- hlaups in Iceland, Global Planet. Change, 35, 255- 271. Bödvarsson, R., S. T. Rögnvaldsson, R. Slunga, and E. Kjartansson (1999), The SIL data acquisition sys- tem at present and beyond year 2000, Phys. Earth Planet Inter., 113, 89-101. Lacasse, C., S. Karlsdóttir, G. Larsen, H. Soosalu, W. I. Rose, and G. J. Ernst (2004 /media/jar/myndsafn/2005EO260001.pdf

• 14. Paper-Olafur-Rognvaldsson_92

  performance of the model. REFERENCES Førland, E. J., Allerup P., Dahlström B., Elomaa E., Jónsson T., Madsen H., Perälä J., Rissanen P., Vedin H. and Vejen F. 1996. Manual for operational cor- rection of Nordic precipitation data. DNMI Report No. 24/96 Klima, 66 pp. Benoit, R., Pellerin P., Kouwen N., Ritchie H., Donaldson N., Joe P. and Soulis E. D. 2000. Toward the use of coupled atmospheric /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 15. Refsgaard_etal-2007-Uncertainty-EMS

  Discrete numerical Categorical Narrative Constant in space and time A1 A2 A3 4Varies in time, not in space B1 B2 B3 Varies in space, not in time C1 C2 C3 It is noticed that the matrix is in reality three-dimensional (source, type, nature). Thus, the categories type and nature are not mutually exclusive, and it may be argued that the ma- trix should be modified in such a way that the two uncer /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 16. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 17. VI_2014_005

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 18. 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

• 19. Journal_of_Hydrology_Veijalainen_etal

  emission scenario were even greater, on average 5.1% units (Fig. 5), indicating that the GCMs are a greater source of uncertainty than the choice of emission sce- nario or RCM. The flow regimes in different regions in Finland are demon- strated with the five example hydrographs of the reference period and of 2070–2099 (Fig. 8a–e, see Fig. 1c for locations). In northern (Fig. 8a) and central (Fig. 8b /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 20. 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