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• 31. CES_D2_2_poster_3x3

  (median) changes from the model-based hindcast. Bottom: the location of the observed change within the hindcast probability distribution. Blue (red) shading indicates areas where the observed change was above the 95th percentile (below the 5th percentile) of the hindcast distribution. These maps show that there was no detailed agreement between the best-estimate precipitation change hindcast /media/ces/CES_D2_2_poster_3x3.pdf

• 32. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 33. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  The well-being of any human community is critically dependent on continued access to natural and man-made resources. Decades before sustainability became a popular slogan, the Ostroms began to investigate the conditions under which natural resources can be man- aged in a sustainable manner. The origins of the Workshop approach can be traced back at least as far as “State Administration of Natural /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 34. Group-1_Scenarios-for-AWM

  t / c o s t ratio H i g h L o w S c enar i o 1 S c ena r io 2 Present time 20302020 Socio E c onomic D e v elopme n t Figure 1. Scenario building for AWM in Horsens Fjord To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments of the productivity of this approach are based on main big strategies which need to have an attention. One of them /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 35. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 36. Isskyrsla_20100407

  N66°44.92' W025°08.94' 79. N66°45.01' W025°08.50' 80. N66°46.32' W025°10.27' 81. N66°46.73' W025°07.19' 82. N66°46.01' W025°04.86' 83. N66°46.22' W025°04.33' 84. N66°47.12' W025°06.45' 85. N66°47.26' W025°04.36' 86. N66°48.44' W025°03.60' 87. N66°49.10' W025°04.45' 88. N66°51.68' W025°03.27' 89. N66°53.36' W024°59.25' 90. N66°55.39' W024°58.89' 91. N66°55.82' W024°58.13' 92. N66°56.15' W025°01.15 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 37. CES_D2.4_VMGO

  the territories of European Russia (ER) and Europe (EU) an ensemble of 9 CMIP3 [1] comprehensive global (coupled atmosphere-ocean) climate models is used in this assessment (Table 1); so called A2 scenario is considered. Both A2 and A1B scenarios are similar in terms of resulting global mean warming up to the mid-21st century IPCC [2]. The projected changes in ER and EU in many cases continue /media/ces/CES_D2.4_VMGO.pdf

• 38. PhD_course-Programme_26Aug2011-final

  Christian Refsgaard, GEUS All week AP Adriaan Perrels, FMI All week SK Sigrún Karsldóttir, IMO All week FU Frederik Uldal, University of Copenhagen Logistic support Course material Papers and book chapters - recommended reading Henriksen HJ, Barlebo HC (2008) Reflections on the use of Bayesian belief networks for adaptive management. Journal of Environmental Management, 88, 1025- 1036. doi:10.1016 /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 39. askja_minnisblad_ens

  and rescue team saw a white plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 40. The weather in Iceland in 2021

  89 54.1 210 129 Sauðanesviti 944.7 107 101 41.8 222 127 Akureyri 636.4 111 98 29.5 172 103 Grímsstaðir 400.4 103 89 14.3 189 97 Skjaldþingsstaðir 1112.4 # 84 61.2 184 115 Dalatangi 1437.2 87 81 47.6 232 145 Höfn í Hornafirði 1327 # 83 /about-imo/news/the-weather-in-iceland-in-2021