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Results:

• 21. 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

• 22. 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

• 23. 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

• 24. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 25. Bárðarbunga 2014 - August events

  colour-code for the Askja volcano remains at ‘yellow'. 29 August 2014 11:58 - The new eruption in Holuhraun Below are two images of the new lava in Holuhraun, ca 5 km north of Dyngjujökull. The images were taken from TF-SIF, the aeroplane of the Icelandic Coast Guard. Later, flowmodels were made. The new lava and steam The new lava that came up in the eruption in the first hours /earthquakes-and-volcanism/articles/nr/3000

• 26. Bardarbunga-2014_August-events

  From the Icelandic Met Office: At 10:00 UTC, IMO changed the Aviation Colour Code for Bárðarbunga to ‘orange', signifying that significant emission of ash into the atmosphere is unlikely. The aviation colour-code for the Askja volcano remains at ‘yellow'. 29 August 2014 11:58 - The new eruption in Holuhraun Below are two images of the new lava in Holuhraun, ca 5 km north of Dyngjujökull /media/jar/Bardarbunga-2014_August-events.pdf

• 27. Bárðarbunga 2014 - August events

  colour-code for the Askja volcano remains at ‘yellow'. 29 August 2014 11:58 - The new eruption in Holuhraun Below are two images of the new lava in Holuhraun, ca 5 km north of Dyngjujökull. The images were taken from TF-SIF, the aeroplane of the Icelandic Coast Guard. Later, flowmodels were made. The new lava and steam The new lava that came up in the eruption in the first hours /earthquakes-and-volcanism/articles/nr/3000/

• 28. VI_2022_006_extreme

  an estimate of uncertainties. Further details can be found in Poli et al. (2016). Data from the ten realizations were retrieved for temperature, total precipitation and snow- fraction for a box around Iceland, extending between latitudes 58 to 72°N and longitudes -5 to -30°W. Data were available from the ECMWF archive at hourly resolution, but for this project, only monthly summed variables were /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 29. 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

• 30. 2010_017

  of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf