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Results:

• 21. ces-glacier-scaling-memo2009-01

  Meteorological Office, Memo ÚR- TóJ-2009-01. AV AILABILITY The gls software can be obtained from Tómas Jóhannesson Veðurstofa Íslands — Icelandic Meteorological Office Bústaðavegi 9 IS-150 Reykjavík Iceland Phone: +354-1-5226000, Fax: +354-1-5226001, E-mail: tj@vedur.is 3 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 22. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  la tio ns hi ps be tw ee n di ffe re nt dis cipline s = > bro ad inte grate d outp ut (bu tn o tq ua nt ita tiv e) Pr ogres s towa rd sIWR M measu re s Ind icator s o fe ffec to f measu res , invo lvin g m o n ito rin g M ul tip le fra m es (so cia l sy st em ):w at er u se s su ch as n av ig at io n , hy dr o ele ct ric po w er ge n er at io n , flo o d pr o te ct io n m u st be ha rm o n ize d w /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 23. 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

• 24. 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

• 25. 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

• 26. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 1 Outline for the case Road maintenance in a changing climate Introduction Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010 /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 27. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 28. VI_2015_005

  in this study, 16 Figure 7. Seasonal per grid point occurrence of low-pressure centres (LPC) for daily av- erages, as well as for 5-day and 31-day running means of daily grid-point time-series. The dotted lines indicate the domain boundaries. The dash-dotted lines indicate bound- aries between different sectors, as described in the text. Note the difference in scale of the colour shading between /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 29. Bárðarbunga 2014 - August events

  line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000

• 30. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf