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• 11. Climate of aerodromes

  BIEG and BIAR based on METAR observations 2001–2010, ANNUAL (pdf 75 Kb). Windrose, average wind speed and gusts Below are pdf-files (0.3 Mb, 17p.) for each airport. BIKF - Keflavik BIRK - Reykjavík BIAR - Akureyri BIEG - Egilsstaðir BIIS - Ísafjörður BIBD - Bíldudalur BIHU - Húsavík BIHN - Höfn BIVM - Vestmannaeyjar BITN - Þórshöfn BIGR - Grímsey BIVO - Vopnafjörður BIGJ - Gjögur Clouds /weather/aviation/climate/

• 12. Benestad_Rasmus_CES_2010

  wind Obs=ERAINT (reanalysis) righttoleftmark Storm statistics Domain: 12°W-38°E/48-66°N (Same as RCM) Historical reanalysis ERAINT Little trend! Historical analysis: N CCI on small domain: restricted RCM domain Domain: 80°W-40°E/20- 75°N Different story! Geographical distribution? Storm statistics: Whole North Atlantic Homogeneous? Historical analysis: |v| Southern Norway SLP 'triangulation /media/ces/Benestad_Rasmus_CES_2010.pdf

• 13. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941

• 14. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 15. Öræfajökull

  was the largest explosive eruption in Iceland in historical time, forming ~10 km3 of silicic tephra. This eruption most likely affected ~75% of the country, but nearby areas were touched the hardest, where total devastation occurred within the 20 km radios of the volcano due to large jökulhlaups (glacial outburst floods), heavy tephra fall, and pyroclastic density currents. The last eruption /volcanoes/about-volcanoes/oraefajokull/

• 16. James-Smith_Edward_CES_2010

  SummerAutumn -Wind power responsible for 75 – 80 % of load --Increased strength of storms means risk of greater fluctuations in wind power production – could require new investments in infrastructure -Warmer winters = lower demand = lower income -Stronger storms = higher tidal flooding which can flood transformers - -Maintenance undertaken in spring – sensitive to large fluctuations /media/ces/James-Smith_Edward_CES_2010.pdf

• 17. Jokull-guidlines

  and subsections should be clearly headed. Tables should be as simple as possible and large tables should be avoided. Each table should have a brief title. All illustrations must be ready for reproduction. The final scale should usually be adjusted either to the width of a single column (75 mm) or the maximum width of the printing area of the page (155 mm). Breadths between /media/jar/Jokull-guidlines.pdf

• 18. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  in order of occurrence, from the first one until the most recent one, which is nr. 75. It is obvious that the time-lapse between such earthquakes increases during this period, and sharply after late October. In other words, large earthquakes have become less frequent. * by Matthew J. Roberts /earthquakes-and-volcanism/articles/nr/3039

• 19. Wind Energy

  Technical University, August 2007. Journal of Physics Conference Series, Vol. 75. 8 pp. Pryor, S. C., Schoof, J. T., Clausen, N.-E. & Drews, M. (2010). Changes in extreme wind and intense wind speeds in Northern Europe. European wind energy conference, Warsaw, April 2010. National Barthelmie, R.J. & Pryor, S. C. (2007). Wind speed trends over the contiguous USA. 30th Annual Applied Geography /ces/publications/nr/1944

• 20. hafisskyrsla_18ag2011

  – 026°19V. 75 sjóm. NV- af Kópanesi. Kl.1337, tveir borgarísjakar á stað: 66°50N 027°21V. Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Kort af ísjökunum út af Vestfjörðum. Flugskýrsla TF-SIF 18. ÁGÚST 2011 Flug nr. 10611.025 Kl. 1400 AIS umferð út af Vestfjörðum og Breiðafirði. Auðunn F /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf