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Results:

• 31. Nordic_Adaption_14_2cir

  Juhola (FIN)  Sigrun Karlsdottir (IS)  Halldór Björnsson (IS)  Richard Klein (S)  Rik Leemans (NL)  Henrik Madsen (DK)  Anil Markandya (E)  Jørgen E. Olesen (DK)  Adrian Perrels (FIN)  John Porter (DK)  Markku Rummukainen (S)  Hans von Storch (D) ORGANIZERS ? S PONSORS 2nd Announcement and Call for Papers 2nd Announcement and Call for Papers www.nordicadaptation2014.net /media/loftslag/myndasafn/Nordic_Adaption_14_2cir.pdf

• 32. Volcanic plumes and tephra

  trajectory. The altitude that the plume can reach depends on several factors, primarily on the mass flux of the eruption. Other environmental factors, like wind field and atmospheric stratification, act on the plume dynamics affecting the final top altitude. Very strong wind can bend the rising mixture causing a lower top altitude and the maximum plume height to be located downwind the eruptive /volcanoes/volcanic-hazards/volcanic-emissions/

• 33. GA_2009_91A_4_Andreassen

  September 2001–10 September 2006 (Andreassen et al. 2008). Thesurface energy balance (SEB) was calculated us-ing an energy balance model previously applied forAntarctica (Van den Broeke et al. 2005). The sur-face energy balance model (hereafter called theSEB-model) calculates the turbulent fluxes, outgo-ing longwave radiation, subsurface heat flux andmelt energy by solving the SEB for the surface tem /media/ces/GA_2009_91A_4_Andreassen.pdf

• 34. Alam_Ashraful_CES_2010

  Time Main assortments l l d Energy biomassSaw ogs Pu pwoo Small trees Residues Stumps 5 Use of biomass based energy in Finland Pellets 1% (0.5 Mm3) S d tForest residues and small trees used as chips 9% (3.4 Mm3) aw us 9% (3.4 Mm3) Black liquorTraditional Energy biomass 46 TWh (55%) qu45% (18 Mm3)firewood 15% (6 Mm3) Bark 21% (8.4 Mm3) Energy biomass: 20% of the primary energy production /media/ces/Alam_Ashraful_CES_2010.pdf

• 35. Hare_2-participation

  Need to quantify and compare risks of doing and not doing participation • Waking sleeping dogs • Process gets delayed powerful stakeholder • Process gets hijacked • Failure to live up to stakeholder expectations 2. Competent Authorities’ Organisational barriers −Departments not communicating, not participating with each other −Planning departments work quicker than participation 3 /media/loftslag/Hare_2-participation.pdf

• 36. Recent publications

  The Icelandic Meteorological Office annually publishes a variety of reports, journals and articles. Below are examples of recent publications, most of which contribute to Arctic issues in general. Large-scale atmospheric conditions associated with major avalanche cycles and cold season weather hazards in Iceland (2013) The wind energy potential of Iceland (2013) Surface wind and air temperature over /about-imo/arctic/completed-projects/publications/

• 37. Statistical Analysis

  by parametric methods. Hydrology Research 39, 425-436. Jónsdóttir, J. F., Uvo, C. B. (2009). Long-term variability in precipitation and streamflow in Iceland and relations to atmospheric circulation. Int. J. Climatol. 29, 425-436. doi: 10.2166/nh.2008.002. Lawrence, D., Haddeland, I. Uncertainty in hydrological modelling of climate change impacts in four Norwegian catchments. Hydrology Research /ces/publications/nr/1943

• 38. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 6 Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired adaptation planning cycle for road transport (at national strategic / tactical level) M a n d a t e f r o m g o v e r n m e n t + p r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 39. Crochet_Philippe_CES_2010

  Impacts of historic climate variations on streamflow characteristics in Icelandic rivers Philippe Crochet Icelandic Meteorological Office Objective • To analyse the hydrologic response of 11 river basins in Iceland to past climate variations, especially temperature variations. • Streamflow characteristics » Discharge seasonality » Mean annual discharge » Number of floods (POT) • Snow storage /media/ces/Crochet_Philippe_CES_2010.pdf

• 40. Factsheet_Bardarbunga_20150130

  large quantities of ice, leading to a major jokulhlaup, accompanied by ash fall. Other scenarios cannot be excluded. NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT Figure 1 A map from January 21st showing the thickness of the lava at Holuhraun, numbers indicate thickness in meters. NATIONAL COMMISSIONER OF THE ICELANDIC /media/jar/Factsheet_Bardarbunga_20150130.pdf