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• 11. BIKF_windrose_2005-2014

  45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 33 2 55 2 79 5 88 3 64 2 42 2 49 4 59 5 52 5 38 3 42 1 40 4 41 0 55 3 63 5 55 6 47 5 39 3 34 6 31 3 33 9 33 9 36 6 48 8 53 9 52 6 47 5 33 6 22 3 19 0 16 4 13 0 9 6 11 6 12 0 15 4 Wind rose BIKF April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIKF_windrose_2005-2014.pdf

• 12. VI_2020_004

  49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 13. Hydropower - Glacier, Snow and Ice

  glacier-scaling-hydrological model. 88-89. Machguth, H., & Ahlstrøm, A. (2010). Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties. p. 42-43. Melvold, K. & Laumann, T. (2010). A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES). 90-91. Radic, V /ces/publications/nr/1940

• 14. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 80/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 15. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  of the three ice caps under consideration, the horizontal displacement of the HRS and DMA DEMs (40 m40 m spatial resolution) relative to the EMISAR DEM (5 m5 m spatial resolution) was eliminated by both maximizing the correlation and minimizing the standard deviation of the elevation differences of ice-free areas in the vicinity of the glaciers (gently sloping areas within ca. 80
  800 m away /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 16. Latest news on the eruption at Reykjanes peninsula

  /about-imo/news/a-new-eruption-has-started-at-fagradalsfjall

• 17. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  but for precipitation changes. Changes in local temperature are strongly controlled by the large-scale temperature change. This is reflected both by the small amplitude of the regression residuals (typically 0.1-0.3°C) and the large explained variance (mostly above 80%, with some exceptions like the Baltic Sea). For changes in precipitation, the correlation between the local and the large-scale changes /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 18. VI_2019_009

  SYNOP codes (manual station): 14, 15 and 16. ................................................................ 25 19 From left to right, the horizontal axis has the following SYNOP codes, in groups (manual station): 21 - 25 - 60,61 - 62,63,92 - 64,65 - 23,68 - 80 - 81. ................ 27 20 From left to right, the horizontal axis has the following SYNOP codes, in groups (manual station): 22 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 19. Snorrason_Arni_CES_2010

  – Energy market aspects • Scale: – Total: 20.8 MNOK – TFI: 12.3 MNOK Estimated Global Sea level rise Vermeer and Rahmstorf 2009 Estimated Global Sea level rise at 2100 Rahmstorf 2010 Deformation of Iceland due to mass loss from glaciers Þ. Árnadóttir et al., GJI, 177 Area of inundation: 1m sea level rise Stability of Arctic Land Ice: SVALI • CES Snow and Ice Group • Many partners from the Nordic /media/ces/Snorrason_Arni_CES_2010.pdf

• 20. ces-oslo2010_proceedings

  Roald, L.A. and Engen-Skaugen, T. Projected effects of climate change on the hydrology of Norway ........................................................................ 80 Duncan, N.J., Harrison, G.P. and Wallace, A.R. Modelling the Scottish hydropower resource ........................................................................................................ 82 Einarsson, B /media/ces/ces-oslo2010_proceedings.pdf