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  • 31. Adalgeirsdottir-etal-tc-5-961-2011

    were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
  • 32. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 33. aerodrome_summaries_20140603

    14 0 1 2 3 8 12 15 0 1 2 3 8 12 16 0 1 2 4 8 12 17 0 1 2 4 8 12 18 0 1 2 4 8 12 19 0 1 2 4 8 13 20 0 1 2 4 8 13 21 0 2 3 5 9 13 22 1 2 3 5 9 13 23 1 2 3 4 9 13 MEAN 1 2 2 4 8 13 10 AE R OD R OM E CLIM A T OLOGICA L SUMMA R Y - T ABL E D AE R OD R OME :BIK F - KEFL A VÍ K /K efl avi k PERIO D O F RECORD :2001–201 0 L A TITUDE :6 3 59’06" N LONGITUDE :2 2 36’20" W ELE V A TIO N AB O V E MSL :5 2 /media/vedur/aerodrome_summaries_20140603.pdf
  • 34. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 35. ces_wind_flyer-hq

    The majority of the grid cells show no significant change, however a rising trend towards the end of the century is noted (red curve). 2071 -2100 relative to 1961-90 [%] Rossby Centre i l d l Declines No change Increases Changes in % for grid cells with significant changes Activities and results reg ona mo e and ECHAM4 Rossby Centre regional model and HadAM3 ECHAM4: A2 0.1 73.2 26.7 ECHAM4: B2 0.1 /media/ces/ces_wind_flyer-hq.pdf
  • 36. Tornado_Impacts_-_FMI_Presentation

    fatalities occurred in mobile homes, although only 7.6% of U.S. housing units in 2000. • A one standard deviation in the proportion of mobile homes in housing stock (8.3 percentage points) increases fatalities by 36% and injuries by 18%. The Mobile Home Problem 50 60 70 80 90 P e r c e n t a g e o f C a t e g o r y F a t a l i t i e s Mobile Homes 0 10 20 30 40 F0 F1 F2 F3 F4 F5 F /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
  • 37. 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
  • 38. VI_2014_005

    %) Subpolar wetlands: 7,208 km2 (7.5%) Subpolar crops: 2,380 km2 (2.5%) Inland water4: 1,463 km2 (1.5%) 4Including also the coastal lagoon Hópið, and the estuary at Höfn. 9 Inland Water Subpolar Wetlands Subpolar Crops Subpolar Pastures Tundra Sparse Tundra Permanent Snow Vatnajökull Mýrdalsjökull Langjökull Hofsjökull Drangajökull Eyja fjall ajö kul l Reykjanesskagi Sp ren gis an du r /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 39. VI2010-006_web

  • 40. VI_2015_005

    at the bound- aries. With longitude, l , parameterised as a function of latitude, f , these boundaries are at l1 = 30 30 40 (f 40) (2) and l2 = 45 90 40 (f 40) : (3) This suggests dividing the study domain into three parts: a western sector, with l < l1, covering the region west of Greenland; a central sector, with l1 l < l2, including the region of the Icelandic Low; and an eastern sector /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

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