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Results:

• 21. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  climate changes between the CMIP3 and ENSEMBLES simulations 15 4. Impact of RCM data on forecasts of climate change 18 5. Probabilistic projections of temperature and precipitation change 24 5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24 5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)? 28 6. Conclusions 34 References /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 22. GA_2009_91A_4_Andreassen

  andminimum bs will be greatly influenced by a warm-ing, but only weakly influenced by increased pre- cipitation (as the bwincreases, but not so much thelength of the season). A warming of 1°C will de- crease (increase) the average day of maximum bw(minimum bs) by 9 and 11 days compared to thereference period (Table 4). For a 3°C warming thelength of the ablation season may increase by c. 50days /media/ces/GA_2009_91A_4_Andreassen.pdf

• 23. CES_D2.4_task1

  KONGSBERG BRANNSTASJON NO +59:37:28 +09:38:16 170 TP 2577 NESBYEN NO +60:34:00 +09:06:00 164 TP 2578 NESBYEN II NO +60:34:00 +09:07:59 165 TP 2579 ROROS AIRPORT NO +62:34:37 +11:21:06 625 TP 2580 RENA NO +61:07:59 +11:22:59 225 P 2581 ONA NO +62:52:00 +06:33:00 /media/ces/CES_D2.4_task1.pdf

• 24. The

  The absoulute maximum temperature of the year was recorded at the station Végeirsstaðir in Fnjóskadal in the East on 25 July, 27.7°C, but the lowest minimum -29.0°C at Svartárkot in the north-eastern upland on 29 December. The absolute maximum in Reykjavík was 22.5°C, recorded on 27 July and the absolute minimum was -8.5°C on 11 December. In Akureyri the maximum was 24.1°C on 22 July /about-imo/news/the-weather-in-iceland-in-2017

• 25. Ved-eng-2006

  Icelandic Meteorological Office – Climate summary 2006 – published 20.2.2007 The weather in Iceland 2006 A summary from the Icelandic Meteorological Office A general overview Figure 1. Teigarhorn in Berufjörður on the east coast on a summer day in August. Photo: Sigvaldi Árnason. The year was generally favourable and warm. In the South and West the temperature was about 1.1°C above /media/vedurstofan/utgafa/skylduskil/Ved-eng-2006.pdf

• 26. hafisskyrsla_04012011

  á meðal Klakkur SH, Sóley Sigurjóns GK og Mánaberg ÓF. Höfðum samband við þessi skip og fengum upplýsingar um sjávarhita og lofthita. Lofthiti var um -3°c og yfirborðssjávarhiti frá -0,9°c við ísröndina upp í plús 7,5°c utan við ísnýmyndun. Semsagt mjög skörp hitaskil og gott fiskerí að sögn skipstjóra á svæðinu. Hafísinn er að þéttleika um 6-8/10 og nýmyndun íss greinileg um 2-3 sjml út frá /media/hafis/skyrslur_lhg/hafisskyrsla_04012011.pdf

• 27. Traffc-maintenance_expenditures

  127 308 1 106 709 2007 .. 611 148 6) 2) 177 646 21 377 4) 30 820 14 021 - 10 141 165 567 319 1 031 039 1 092 234 2006 .. 612 044 6) 2) 113 312 22 002 4) 34 446 14 868 - 15 888 151 738 368 964 666 1 070 901 2005 .. 599 686 5) 2) 154 481 28 661 4) 27 846 13 748 - 12 079 159 879 379 996 759 1 169 271 2004 .. 587 176 2) 141 446 59 834 4) 24 546 10 342 - 6 326 164 502 573 994 745 1 226 881 2003 .. 627 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 28. Eyjafjallajokull_status_2010-05-03_IES_IMO

  (16:00 GMT). Noises: Scientists working at Gígjökull regularly hear explosions and booming sounds and feel the ground vibrate. The vibrations are not felt in 3-4 km distance. Additional note: The scientists at Gígjökull experienced discomfort due to gas. Meltwater: Today water temperature at the Markarfljot bridge was measured 11°C but about 3°C in a 2 km distance from Gígjökull. Water /media/jar/Eyjafjallajokull_status_2010-05-03_IES_IMO.pdf

• 29. Cradden_Lucy_CES_2010

  ? • Based on thermodynamic and heat transfer models accounting for: Wire resistance Solar heating Radiative cooling Convective cooling June 2010 7 How are ratings determined? • UK network standards assume seasonal average temperatures and worst-case wind conditions, i.e. low wind speeds Summer → 20˚C; Spring/Autumn → 9˚C; Winter → 2˚C • Real-time monitoring (‘dynamic rating’) is not commonly /media/ces/Cradden_Lucy_CES_2010.pdf

• 30. 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