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Results:

• 11. vanRoosmalen_etal-2009-WRR_2007WR006760

  water model, which makes it possible to include feedback processes of the simulated changes. 2. Study Area [9] The study area is located in the western part of Jutland, Denmark, between the Jutland Ridge and the west coast (Figure 1) with an area of 5459 km2. The topography slopes gently from east to west with land surface elevations from 125 masl in the eastern part to sea level at the coast. Land /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 12. Kriauciuniene_Jurate_CES_2010

  of temperature anomaly (ºC) between 1991-2007 and 1961-1990 Variation of annual T anomaly (ºC) between 1991-2007 and 1961-1990 Seasonal differences of P anomaly (in %) between 1991-2007 and 1961-1990 Seasonal differences of Q anomaly (in %) between 1991-2007 and 1961-1990 Variation of annual P and Q anomaly (%) between 1991-2007 and 1961-1990 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 /media/ces/Kriauciuniene_Jurate_CES_2010.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. 42nd Nordic Seismology Seminar

  Grensásvegur 9 (see Transportaion). Organized by: Icelandic Meteorological Office, Institute of Earth Sciences, University of Iceland, Iceland Geosurvey and Reykjavík University. Perlan in Öskjuhlíð. The photograph is taken from the Meteorological Office 10 February 2009 at 9:14 by Helgi Borg Jóhannsson /norsem/

• 15. 42nd Nordic Seismology Seminar

  Grensásvegur 9 (see Transportaion). Organized by: Icelandic Meteorological Office, Institute of Earth Sciences, University of Iceland, Iceland Geosurvey and Reykjavík University. Perlan in Öskjuhlíð. The photograph is taken from the Meteorological Office 10 February 2009 at 9:14 by Helgi Borg Jóhannsson /norsem

• 16. VI_2020_005

  00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Guðrún Elín Jóhannsdóttir, Department of Earth Sciences at Uppsala University Abstract Flood risk increases with rising sea levels and coastal settlements need to adapt to this increasing risk. For that, hazard and risk assessments are an important step. Coastal floods have caused prob- lems in Iceland in the past /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 17. 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

• 18. Measurement results

  Measurement results © Míla An image from the web cam of Míla, taken 9 December 2014 at 16:11 /pollution-and-radiation/volcanic-gas/measurements/bigimg/3036

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

  lines of the fu- ture climate provides an implicit bias correction (Jóhannes- son et al., 2011). Figure 9 shows the simulated annual mean temperature and precipitation averaged over Iceland for the 13 scenarios used in this study, compared with the average 2000–2009 climate. All the scenarios indicate a slight in- crease in the precipitation during this century (∼10 %) and a warming of 1.1–1.5 ◦C /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 20. BIHN_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 68 0 62 9 111 2 167 0 117 5 70 6 26 7 25 4 58 7 47 3 36 6 101 3 91 1 53 1 117 0 73 6 44 2 72 7 38 7 60 4 113 6 70 0 109 3 130 5 26 1 12 5 30 0 14 4 10 5 34 6 17 0 29 4 114 3 158 0 146 5 172 7 Wind rose BIHN January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIHN_windrose_2005-2014.pdf