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Results:

• 1. Traffc-maintenance_expenditures

  047 13 903 11 197 - - - 522 610 1 406 449 1980 42 409 153 761 14 024 212 220 - 5 257 17 816 10 410 9 234 - - - 465 133 1 420 546 Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land /media/loftslag/Traffc-maintenance_expenditures.pdf

• 2. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 3. 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

• 4. 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

• 5. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 6. 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

• 7. 2010_005_

  Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century Nikolai Nawri Halldór Björnsson VÍ 2010-005 Skýrsla Surface Air Temperature and Precipitation Trends for Iceland in the 21st Century VÍ 2010-005 ISSN 1670-8261 Skýrsla +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Nikolai Nawri, Icelandic Meteorological Office Halldór /media/ces/2010_005_.pdf

• 8. VI_2015_009

  Regional Flood Frequency Analysis: Application to partly glacierized and/or groundwater-fed catchments Philippe Crochet VÍ 2015-009 Report Regional Flood Frequency Analysis: Application to partly glacierized and/or groundwater-fed catchments VÍ 2015-009 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Philippe Crochet, Icelandic Met Office /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 9. VI_2009_006_tt

  Íslands Bústaðavegur 9 150 Reykjavík   Abstract Fast-rising jökulhlaups from the geothermal subglacial lakes below the Skaftá caul- drons in Vatnajökull emerge in the Skaftá river approximately every year with 45 jökulhlaups recorded since 1955. The accumulated volume of flood water was used to estimate the average rate of water accumulation in the subglacial lakes during the last decade as 6 Gl /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 10. VI_2014_006

  Probabilistic daily streamflow forecasts based on the combined use of a hydrological model and an analogue method Philippe Crochet VÍ 2014-006 Report Probabilistic daily streamflow forecasts based on the combined use of a hydrological model and an analogue method VÍ 2014-006 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 150 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf