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  • 1. Traffc-maintenance_expenditures

    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 grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /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. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

    assessments in coastal and marine tourism”, Proceedings of CMT2009, the 6th International Congress on Coastal and Marine Tourism, South Africa 23-26 June. Available at: http://www.cmt2009.com/Proceedings/content/CMT2009_WP_039.pdf, 22 June 2010. [4] Ehmer, P. and Heymann, E. (2008): “Climate change and tourism: Where will the journey lead?” Deutsch Bank Research, April 11, 2008. Available /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
  • 4. IMO_AnnualReport2014

    of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 5. Refsgaard_etal-2007-Uncertainty-EMS

    the model. Usually, the model is run within a graphical user interface (GUI) where many tasks have been automated.  STEP 4 (calibration and validation). This step is con- cerned with the process of analysing the model that was constructed during the previous step, first by calibrating the model, and then by validating its performance against independent field data. Finally, the reliability of model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 6. Irafossmyndir_1-4

     Mynd 1  Mynd 2  Mynd 3  Mynd 4 /media/geislun/myndasafn/Irafossmyndir_1-4.doc
  • 7. 2005EO260001

    lake within the caldera until the surrounding ice is breached. When that happens, water escapes to cause a jökulhlaup in the river Skeidará, after having traveled ~50 km beneath the Skeidarárjökull outlet glacier (Figure 1b). Jökulhlaups occur there every 1–10 years and last from days to weeks, each time releasing 0.4–4 km3 of water [Björnsson, 2002]. Volcanic eruptions in Gríms- vötn often /media/jar/myndsafn/2005EO260001.pdf
  • 8. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 9. vanRoosmalen_etal-2009-WRR_2007WR006760

    have a consider- able impact in an area where surface runoff is the dominant process, but have a smaller impact on groundwater-fed systems. Owing to the heterogeneity of the meteorological conditions and the heterogeneous physiographical condi- tions, climate and land use change impact studies on hydrology often have a local to regional character. [4] The majority of hydrological climate change /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 10. VED_AnnualReport-2013_screen

    and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

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