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• 31. ces-glacier-scaling-memo2009-01

  Memo ÚR–TóJ–2009–01 A simple (simplistic) method to include glaciated areas with a limited ice volume in the WaSiM and HBV models Tómas Jóhannesson 5.12.2009 Background Within the CES project, there is a need for simple runoff modelling of drainage basins with many glaciers without detailed mass balance and dynamic modelling of each glacier. Such modelling needs to take into account the limited /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 32. Climate change and hydrology: Environmental and societal effects

  will increase by 20%. The current system can only utilize less than half of this energy increase due to its limited capacity. These results must be applied when redesigning and upgrading the hydropower plants. Effects on sea level Regional scenarios have been made for changes in sea level due to climate change where the estimated sea level in 2081-2100 is compared to the sea level in 1986-2005 /about-imo/news/nr/2910

• 33. QA on the eruption in Eyjafjallajökull 2010

  the eruption and the ash plume (pdf 1,5 Mb). Why were there floods? Can floods always be expected? Several very sudden jökulhlaups (glacier outburst floods) have occurred during the subglacial eruption in Eyjafjallajökull volcano. The largest one came in the very beginning of the event with maximum discharge about 2000-3000 m3/sec. Now the eruption is constrained to one vent and, therefore, very limited /earthquakes-and-volcanism/articles/nr/1880

• 34. Alam_Ashraful_CES_2010

  Source: Finnish Forest Research Institute, 2007 6 Interactions: forests, climate, management &production  Boreal forests: growth is mainly limited by low temperature, short growing season  Climate change effect: defined by increase in temperature, precipitation and CO2, may provide favourable condition to boreal forests to grow forest faster  Management: expected climate change may bring a new /media/ces/Alam_Ashraful_CES_2010.pdf

• 35. Lawrence_Deborah_CES_2010

  are likely to be impacted by climate change: Runoff from rainfall and/or snowmelt Excess rainfall in areas with limited infiltration Intense precipitation in localised areas Photo: NVE Manndalen, May, 2010; Photo: NVE Hønefossen, May, 2008; Photo:NVE Modelling chain for hydrological impact projections /media/ces/Lawrence_Deborah_CES_2010.pdf

• 36. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 37. Hare_1_PartINONAM

  monitoring Public involvement campaigns • moderated activity with a limited number of participants in which participants work together to carry out a common task » Nominal Group Technique, Participatory modelling (e.g. group model building), Role playing games, Scenario building, Forum theatre, Participatory budgeting.... Workshops / Collaboration Taken from Hare & Krywkow, (2004) Matching classes /media/loftslag/Hare_1_PartINONAM.pdf

• 38. VI_2015_006

  intensity is given as the sine of the al- titude angle. Absolute incident solar intensity at the top of the atmosphere is obtained by multiplication with 1360 W m 2. Rise [UTC] Set [UTC] Length [hrs] Noon [UTC] Altitude [deg] Intensity 27 Jul 2012 03:58 22:46 18:48 13:22 44.05 0.70 3 Aug 2012 04:22 22:21 17:59 13:22 42.32 0.67 3 Sep 2012 06:03 20:27 14:24 13:15 32.30 0.53 16 are limited to about 50 W /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 39. Paper-Olafur-Rognvaldsson_91

  is done by using the mesoscale MM5 model (Grell et al., 1995). This paper begins with a description of the model approach, followed by comparison of the model results to data and concluding remarks. MODELLING WITH THE MM5 MODEL The idea of using limited area models (LAMs) for regional climate simula- tions was introduced by Dickinson et al. (1989) and refined by Giorgi (1990). One of the benefits /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 40. Hydropower - Glacier, Snow and Ice

  ). Reykjavík, The Ministry for the Environment. [This report is not a deliverable of the CES-project, but it is partly based on work that was carried out within the CE and CES-projects, in particular the work of the glaciers/snow and ice groups.] Jóhannesson, T. (2009). A simple (simplistic) method to include glaciated areas with a limited ice volume in the WaSIM and HBV models. Icelandic Meteorological /ces/publications/nr/1940