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Results:

• 11. Hare-2011-ParticipatoryModelling

  support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 12. VI_2009_006_tt

  the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 13. Observations - Eskifjörður

  Observations - Eskifjörður | Observations | Icelandic Meteorological office Observations - Eskifjörður Mon 1.05 14 GMT 4.6° S 6 Max wind : 7 / 12Precip.: 0.0 mm / 1 h 13 GMT 4.8° SSW 6 Max wind : 6 / 10Precip.: 0.0 mm / 1 h 12 GMT 4.5° SSW 5 Max wind : 8 / 10Precip.: 0.0 mm / 1 h 11 GMT 4.2° S 7 /m/observations/areas

• 14. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 15. Adalgeirsdottir-etal-tc-5-961-2011

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 16. Journal_of_Hydrology_Veijalainen_etal

  24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 17. 2015-03-12_vatnsvedurogstormar_en

  weather forecast: Two low pressure systems are forecast to reach Iceland during the period from Friday morning until Saturday evening. The forecast is for southeast 20-25 m/s, (strong gale to storm) tomorrow, Friday, but south 25-30 m/s (storm to violent storm) on Saturday. A heavy rainfall warning has also been issued for these lows.. Travel conditions will be poor in the south and west /media/frettir/myndasafn/2015/2015-03-12_vatnsvedurogstormar_en.pdf

• 18. VI_2020_005

  exist that reach back to early 19th century but most series are much shorter (Hamlington and Thompson, 2016). In contrast, satellite altimetry has only been available since the early 1990’s. Satellite altimetry mea- sures the sea surface height, namely the sea level compared to a fixed reference frame (the center of the earth, the geoid or a reference ellipsoid) for latitudes up to 66 N and S (ESA /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 19. Low level flight conditions over Iceland

  -13 FL180: 270/25-45KT, but 26015KT by the NE-coast, -29 Overview of weather systems: 1000 km S of Cape Farewell is an extensive 980 mb low. Over Greenland is a 1038 mb high. Near surface winds: N-ly or variable wind, 05-25 KT. Cloud heights/visibility/weather: BKN/OVC at 1000-2500 FT in the N-part and occasional snowshowers with poor visibility. Widely FEW/SCT and good /weather/aviation/llf-iceland/

• 20. Warning due to gale winds and heavy precipitation

  Warning due to gale winds and heavy precipitation 20.7.2012 Saturday afternoon and evening, 21st July, strong southeast- and easterly winds are expected in the southern and western parts of Iceland with heavy rain. Mean wind speed will be 13 to 20 m/s and occasional /about-imo/news/nr/2501