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  • 31. Alam_Ashraful_CES_2010

    dimension to current mgt. as it utilises the opportunity provided by the surrounding environment  Energy biomass production 7 What are the challenges?  EU is committed to raise the share of renewable energy to 20% by 2020  This target for Finland is 38% by 2020  The production of energy biomass to substitute fossil fuels I 2006 21 il 3 (46 TWh) f bi d i  n 200 , 21 m . m o energy /media/ces/Alam_Ashraful_CES_2010.pdf
  • 32. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 33. Factsheet-Bardarbunga-140904

    km of altitude. The volcanic cloud will drift towards south in the coming hours due to wind rotation.  Four scenarios are likely: o The migration of magma could stop, resulting in a gradual reduction in seismic activity and no further eruptions. o The dike could reach the Earth’s surface causing another eruption, possibly on a new fissure. Lava flow and (or) explosive activity cannot /media/jar/Factsheet-Bardarbunga-140904.pdf
  • 34. NONAM_1st_workshop_summary_v3

    Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H., 2010: Climate Change and Freight Transport. Ministry of Transport and Communications – publication 15/2010. 98 pp. (in Finnish, abstract in English). NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary 9 Text box – questions on which was deliberated in both parallel sessions 1. Which stakeholders should be involved /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
  • 35. Group-1_Scenarios-for-AWM

    example can be given by the low cost still flood risk adaptation by implementing early warning system. But there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens. Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 2 / 3 R es e a r c h Flood f r equenc y a n d i n t ensi t y c o m m un i c a t /media/loftslag/Group-1_Scenarios-for-AWM.pdf
  • 36. AnneFleig_May2010_CES

    activities. Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “ University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook Hydrological drought in NW-Europe: Data 5 6 5 8 6 0 5 5 . 5 5 6 . 0 5 6 . 5 5 7 . 0 5 7 . 5 -10 -5 0 5 10 15 20 25 3 5 4 0 4 5 5 0 5 5 6 0 6 5 7 0 s o u r c e : N a t i o n a l E n v i r o n m e n t a l R e s e a r /media/ces/AnneFleig_May2010_CES.pdf
  • 37. Hydropower - Glacier, Snow and Ice

    of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.). Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1. Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I /ces/publications/nr/1940
  • 38. Factsheet_Bardarbunga_20141203

    the last 100 years. The findings of the meetings are as follows: o Earthquakes in Bardarbunga: Seismic activity has been very strong since mid-august. The activity peaked in first half of September, it has slowly decreased since then, but activity remains intense. The period of seismic unrest is one of the largest ever recorded in a volcano globally. o Earthquakes in the dyke from Bardarbunga /media/jar/Factsheet_Bardarbunga_20141203.pdf
  • 39. VI_2015_009

    vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 40. Avalanche dams

    ofan byggðarinnar. (Náttúrufræðingurinn, 69, 1, 3−10, 1999, authors T. Jóhannesson, O. Pétursson, J. G. Egilsson and G. G. Tómassson) [abstract] (html) A map on a selected front page shows recent observations of avalanches. For user access to avalanche and landslide data, an avalanche map viewer is available /avalanches/imo/dams/

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