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Results:

• 11. 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

• 12. vanRoosmalen_etal-2009-WRR_2007WR006760

  for Denmark [Scharling, 1999] providing daily values for temperature, precipitation, and reference evapo- transpiration ETref (potential evapotranspiration for a well watered grass of uniform height) at a 40-km resolution. For each grid cell representative time series are estimated on the basis of data from available climate stations. For this study we have retrieved data for the period 1990–2004 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 13. ces-oslo2010_proceedings

  ................................................... 40 Machguth, H. and Ahlstrøm, A. Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties ..................................................................................................................................... 42 CLIMATE CHANGE EFFECTS ON RENEWABLE ENERGY Mo, B., Wolfgang, O. and Styve /media/ces/ces-oslo2010_proceedings.pdf

• 14. Reykholt-abstracts

  elevations in the Weddell and Bellingshausen seas Hrafnhildur Hannesdóttir, Helgi Björnsson, Finnur Pálsson and Snævarr Guðmundsson .................................................................................................................................................. 40 Glacier surface elevation changes in the accumulation area of Vatnajökull ice cap since the end of the Little Ice Age /media/vatnafar/joklar/Reykholt-abstracts.pdf

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

  of the glacier is projected to be reduced by 30 % with respect to the present at the end of this century. If the climate warms, as suggested by most of the climate change scenarios, the model projects this glacier to almost disappear by the end of the 21st century. Runoff from the glacier is predicted to increase for the next 30–40 yr and decrease after that as a consequence of the diminishing ice-covered area /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 16. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 17. Case_A___Horsens_Fjord

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/Case_A___Horsens_Fjord.pdf

• 18. Horsens_case

  fiord area. Adaptive challenges due to changes in regional groundwater level An increase in sea level will cause more frequent flooding in the town due to its low lying position by the fjord. In 2006, the local town hall was flooded when sea level rose to 1.76 m above normal. Simultaneously, increased net precipitation and increased rainfall intensity put pressure on the sewage system /media/loftslag/Horsens_case.pdf

• 19. Bárðarbunga 2014 - August events

  do not allow overflight at this time. The opportunity to fly over the area will be assessed later today. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga is at ‘red' and the code for Askja at ‘yellow'. 31 August 2014 08:40 - Eruption in Holuhraun observed 05:15 Observation from scientists in the field (05:15): It appears that the eruptive fissure is longer than /earthquakes-and-volcanism/articles/nr/3000

• 20. Bardarbunga-2014_August-events

  are in the area, using every opportunity to acquire information on gas and lava outflow.  Weather conditions do not allow overflight at this time. The opportunity to fly over the area will be assessed later today. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga is at ‘red' and the code for Askja at ‘yellow'. 31 August 2014 08:40 - Eruption in Holuhraun observed 05:15 /media/jar/Bardarbunga-2014_August-events.pdf