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Results:

• 31. Horsens_case

  in mean values) • Increased wind and higher variability in velocities (4 % more wind and 10 % increase in the strength of storms) NONAM Summerschool Copenhagen 22-26 August 2011 4 • Increased precipitation and higher variation (+ 15 % in average precipitation, 43 % more rain in winter) • More extreme events • Increased sea level (between 0.9 and 1.6 m) • Increased groundwater levels in most /media/loftslag/Horsens_case.pdf

• 32. VI_2015_009

  J600v berg 2.utg) were also used in this study. Table 1. Main characteristics of river basins used in this study. River Name Type Area Mean Percentage Mean annual Period / (km2) elevation glacier precipitation for Gauging (m a.s.l) (mm) streamflow station (1961-2014) data vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014 vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014 vhm66 Hvítá (Borgarfirði) L+J 1577 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 33. 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

• 34. 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

• 35. 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

• 36. 2010_016

  .................................................................................................................... 7 2 INTRODUCTION ........................................................................................................... 8 3 METHODS .................................................................................................................... 10 4 DATA /media/ces/2010_016.pdf

• 37. VI_2014_006

  The analogue method.............................................................................. 9 2.2.1 Principle and background .............................................................. 9 2.2.2 Prerequisites............................................................................... 10 2.2.3 Predictors .................................................................................. 11 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 38. VI_2022_006_extreme

  no direct glacial influence within its catchment. The glacial cover varies greatly between the catchments, reaching 74% for Hálslón, the only one with a glacial coverage above 50%. Three other catchments have glaciers occupying more than 10% of their surface: Hágöngulón, Sultartangi, and Ufsarlón. Table 1 – Properties of the eleven hydropower catchments. Note that the values are derived from /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 39. Bardarbunga-2014_August-events

  activity. * The intrusion reaches the surface and an eruption occurs again where either the fissure is partly or entirely beneath Dyngjujökull. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. At 10:00 UTC, IMO changed the Aviation Colour Code for Bárðarbunga to ‘orange', signifying that significant emission of ash into the atmosphere /media/jar/Bardarbunga-2014_August-events.pdf

• 40. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf