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  • 41. 2013_001_Nawri_et_al

    . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 67 A.14 Þorlákshöfn . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 69 5 List of Figures 1 Topographic map of Iceland with the locations of test sites . . . . . . . . . . . . . 10 2 Annual modelled wind speed distributions and Weibull fits . . . . . . . . . . . . . 16 3 Annotated example of a wind atlas (.lib) text file /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 42. Öræfajökull : Recent research

    of the chapters can be downloaded or short summaries read.Downloadable material:Full text (pdf 23 Mb)Front matter (pdf 180 Kb)Table of contents (pdf 7.9 Kb)Chapter I. Volcanogenic floods in Iceland: An exploration of hazards and risks (pdf 1.06 Mb)Pages 7–16Emmanuel Pagneux, Sigrún Karlsdóttir, Magnús T. Gudmundsson, Matthew J. Roberts og Víðir ReynissonShort summaryChapter II. Öræfajökull Volcano /volcanoes/about-volcanoes/oraefajokull/new-research/
  • 43. 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
  • 44. M5.6 at the Reykjanes peninsula

    M5.6 at the Reykjanes peninsula The largest earthquake measured since 2003 27.10.2020 Updated 27.10.2020Seismic activity has decreased significantly in recent days. About 180 earthquakes of magnitude 2.2 or less were detected the last two days /about-imo/news/m56-at-the-reykjanes-peninsula
  • 45. Dataseries and components

    ), quantity (mm), pH Heavy metals in aerosol: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/m3) Cl, NO3-N, SO4-S (µg/m3) Hg (pg/m3) Persistent organic pollutants (POPs), same for precipitation (ng/l) and air (pg/m3): alfa-HCH, beta-HCH, gamma-HCH p,p'-DDE p,p'-DDD o,p'-DDT p,p'-DDT dieldrin HCB cis-chlordan, trans-chlordan, trans-nonachlor, PCB-28, -31, -52, -101, -105, -118, -138, -153, -156 /pollution-and-radiation/pollution/components/
  • 46. Factsheet_Bardarbunga_20141210

    into the small island in the centre of the lava field. This change can be seen from web cameras.  Seismic activity in Bardarbunga continues to be strong. The strongest earthquake since noon on Monday, 8. December, was magnitude M4,9 on Tuesday at 18:00. About 20 earthquakes larger then M3,0 were detected since Monday. In total about 180 earthquakes were detected in Bardarbunga since noon on Monday /media/jar/Factsheet_Bardarbunga_20141210.pdf
  • 47. VI_2019_009

    Only 17% of the records are nonsensical where the auto- matic station is showing clear, mist, fog or snow while the manual station is showing drizzle. The automatic station also shows drizzle in 14% cases (green) and most cases are blue, 69%, where the automatic station is showing rain or rain showers. In 14 cases the automatic station shows clear while the manual station shows drizzle (slight /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 48. VI_2009_006_tt

    . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 63 8 Conclusions 67 References 69 x List of Figures 3.1 Overview map of western Vatnajökull. . . . . . . . . . . . . . . . . . 10 3.2 The Skaftá cauldrons. . . . . . . . . . . . . . . . . . . . . . . . . . . 11 3.3 Discharge in the 2006 and 2008 jökulhlaups from the Eastern Skaftá cauldron /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 49. CES_D2.4_task2_CMIP3_winds

    in the Nordic area in its western parts (Denmark, west coast of Sweden and western Norway up to 69°N). Along with the simulated warming of the climate, the wind speeds increase in the southern part of northern Europe, the average Vg over the southern Baltic Sea being 9,5-10 m/s in the period 1971-2000 and 10-10,5 m/s in 2046-2065. 3 Fig. 2. 10-GCM mean of the simulated geostrophic wind speeds /media/ces/CES_D2.4_task2_CMIP3_winds.pdf
  • 50. VI_2015_005

    model grid point must be taken into account. At latitude f , the grid-box size is given by dA = a2 cosf dldf ; (1) where a = 6371 km is the Earth’s mean radius, and latitude and longitude are measured in radians. For the ECMWF reanalyses, angular grid-point spacing dl = df = p=180 is constant across the domain. The low-pressure centre count at each grid point is then multiplied by dA=dA, with mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

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