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  • 21. Sea ice in April 2011

    was seen just within the jurisdiction of Greenland. No large floes were seen on radar beyond the ice edge. No observations were received from ships but 3rd April one observation was received from land, reporting an ice berg in location 65°42' N 32°07'W. On the Greenland Straight easterlies were predominant but occasionally strong southwesterly wind prevailed for a few days /sea-ice/monthly/2011/nr/2375
  • 22. ces_SA_group_flyer_new

    series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf
  • 23. BIGJ_windrose_2005-2014

    W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 35 62 48 77 8 4 83 63 64 22 19 14 7 4 11 11 14 41 1 5 24 25 18 45 64 41 3 2 93 35 11 17 7 11 47 16 24 67 36 Wind rose BIGJ January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 Frequency of wind /media/vedur/BIGJ_windrose_2005-2014.pdf
  • 24. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 25. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

    296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf
  • 26. BIBD_windrose_2005-2014

    W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 36 2 69 4 138 2 187 3 151 2 106 7 83 1 58 1 36 0 20 3 17 6 14 5 14 9 11 0 10 6 13 0 16 7 29 8 55 2 73 0 95 6 140 7 98 9 41 9 20 2 17 7 8 1 6 4 4 8 3 7 5 7 4 4 4 5 7 3 9 2 18 5 Wind rose BIBD January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIBD_windrose_2005-2014.pdf
  • 27. BIIS_windrose_2005-2014

    Wind rose BIIS 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 33412 Calm: 12% Variable winds: 11% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W N /media/vedur/BIIS_windrose_2005-2014.pdf
  • 28. Lorenzoni_Pidgeon_2006

    level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 29. Hofsjökull ice-cap

    NASA USGS, shows the northern half of the ice cap Hofsjökull (enlarge). A new patch, visible at the bottom of the image (see arrow), has now been confirmed as a cauldron (~64°49,5‘N; 18°52‘W) at around 1700 m above sea level. Below is a map of Iceland with Hofsjökull tagged (maps.google.com). Travellers are advised to be very careful during journeys on Hofsjökull. Crevasses surround the new /about-imo/news/nr/2768
  • 30. Largest earthquakes during the last 48 hours

    2.030.04 14:11:0730.63.5 km NE of Básar 1.830.04 00:26:13Check.33.1 km ESE of Grímsey 1.730.04 02:16:01Check.3.8 km ESE of Bárðarbunga 1.630.04 13:25:0090.04.1 km W of Dreki 1.529.04 16:47:58Check.5.7 km ENE of Goðabunga 1.329.04 16:13:22Check.17.5 km E of Grímsey 1.230.04 00:49:27Check.33.9 km ESE of Grímsey Sitemap Front page /m/earthquakes/largest

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