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Results:

• 31. Violent storm expected in the South

  Violent storm expected in the South 3.12.2015 A strong gale warning (average windspeed above 20 m/s) is effect in Iceland on Friday afternoon, and a violent storm (average wind speed, above 28 m/s) is expected in the southern /about-imo/news/nr/3242

• 32. Strong gales

  9th, lasting well into Saturday morning. Wind speeds measuring 20 m/s and higher were recorded at half of the automatic weather stations in the lowland areas and similar speeds were recorded at 80% of automatic weather stations in the highland areas. In the town of Heimaey in the Westman Islands, wind-speed* of 28 m/s and gusts measuring 45.8 m/s were recorded at the height of the storm, setting /about-imo/news/nr/1732

• 33. Strong gales

  A great storm passed over Iceland on Friday night, October 9th, lasting well into Saturday morning. Wind speeds measuring 20 m/s and higher were recorded at half of the automatic weather stations in the lowland areas and similar speeds were recorded at 80% of automatic weather stations in the highland areas. In the town of Heimaey in the Westman Islands, wind-speed* of 28 m/s /about-imo/news/nr/1732/

• 34. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf

• 35. Alam_Ashraful_CES_2010

  FOREST BIOMASS FOR ENERGY PRODUCTION – POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki School of Forest Sciences, University of Eastern Finland, Joensuu F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on Oslo, Norway 2 June, 2010 Contents • Forestry in Finland • Challenges • Objectives /media/ces/Alam_Ashraful_CES_2010.pdf

• 36. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 37. Festive forecast

  -13 m/s with sleet or intermittent rain, but in the afternoon lighter winds are forecast in northern and eastern Iceland with brighter skies. At midnight winds will be calm everywhere, although light snow showers are expected in the south and the west. Temperatures will be close to zero. New Year‘s Day has also a fine weather forecast, given the season; slow wind, scattered hail and 0°C. Some /about-imo/news/nr/3053

• 38. VI_2019_009

  with the following equation, h = c t 2 where c is the speed of light (c = 2.99 x 108 m/s). In principle, CL51 is able to detect three cloud layers simultaneously, but if the cloud base is obscured due to precipitation or ground-based fog, vertical visibility is reported. Information about fog and precipitation can also be derived from the return signal as they attenuate the return signal from a cloud. In its /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 39. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  4. critical thresholds & linking multiform uncertainty 5. appropriate spatial scales & combining certified and tacit knowledge Initial session allocation for 1st round review session: Participating PhD Students responsiveness community based adaptation transparency & information access critical thresholds appropriate spatial scales economic (s ctor) impacts indicator choice uncert /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 40. 2013_001_Nawri_et_al

  over complex terrain. On sunny and otherwise calm days, wind speeds associated with sea breezes can reach up to 10 m s 1 at various locations around the Icelandic coast (Einarsson, 1976). Land 11 breezes occur less frequently and are generally weaker. On intermediate time-scales of several days, temporal variability is primarily due to the evolution and passage of cyclonic storm systems. Cyclones /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf