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Results:

• 11. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Icelandic glaciers. Jo¨kull 58, 365
  386. Bjo¨rnsson H., Pa´lsson F. & Haraldsson H.H. 2002. Mass balance of Vatnajo¨kull (1991
  2001) and Langjo¨kull (1996
  2001), Iceland. Jo¨kull 51, 75
  78. Bouillon A., Bernard M., Gigord P., Orsoni A., Rudowski V. & Baudoin A. 2006. SPOT 5 HRS geometry performance: using block adjustments as a key issue to improve quality of DEM generation. ISPRS Journal /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 12. 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

• 13. 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

• 14. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 15. IMO_AnnualReport2014

  or not, is yet to transpire. But at least the exten- sive monitoring of this rifting event makes it quite unique. An intense earthquake swarm began in the Bárðarbunga caldera on 16 August 2014. During the next two weeks, a magma intrusion formed a 49 km long dyke in the upper crust. It migrated from the caldera to Holuhraun, where a fissure eruption commenced at the end of August. This eruption /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 16. 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

• 17. 2005EO260001

  coincide with jökulhlaups. Monitoring Systems To monitor seismic and volcanic activity in Iceland, IMO operates a nationwide digital network of 44 seismic stations (network name: SIL) [Bödvarsson et al., 1999], six volumetric borehole strain meters, and 16 continuous GPS stations (network name: ISGPS) (H. Geirs- son et al., Current plate movements across the Mid-Atlantic Ridge determined /media/jar/myndsafn/2005EO260001.pdf

• 18. VI_2014_005

  Differences in terrain elevation between HARMONIE model and DEM............. 12 4 Dependence of temperature and wind speed on model terrain elevation.............. 13 5 Average diurnal cycles of HARMONIE model temperature and wind speed........ 14 6 Absolute mean errors of SURFEX 2-m air temperature and 10-m wind speed ..... 16 7 Average profiles of air temperature and wind speed in January /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 19. 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

• 20. VI_2020_005

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16 2.2.1 Sea level data for Scandinavia, the UK and Iceland . . . . . . . . . . . . . 17 2.3 Observed sea level changes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 2.3.1 Observed sea level changes in Scandinavia, the UK and Iceland . . . . . . 21 2.4 Sea level projections /media/vedurstofan-utgafa-2020/VI_2020_005.pdf