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Results:

• 51. 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

• 52. The weather in Iceland in 2021

  station total mm 1991-2020% 2011-2020 % max 24-hr mm prec.days >=1.0 mm Reykjavík 765.3 87 82 18.6 232 150 Stykkishólmur 675.7 92 88 29.9 211 124 Hólar í Dýrafirði 1237.3 # 105 112 235 132 Litla-Ávík 836.2 # 92 45.7 225 145 Skeiðsfoss 915.6 94 /about-imo/news/the-weather-in-iceland-in-2021

• 53. BIGJ_windrose_2005-2014

  direction (%) Aerodrome Total observations: 88 Calm: 1.1% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 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 5 5 4 7 13 7 5 1 1 1 1 2 2 4 2 2 4 7 1 2 1 8 2 Wind rose BIGJ June /media/vedur/BIGJ_windrose_2005-2014.pdf

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

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 55. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf

• 56. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 57. Bardarbunga_kafli20140825

  systems in Iceland during the past 11 centuries: frequency, periodicity and implications. In Smellie JL and Chapman MG (eds): Volcano-Ice Interactions on Earth and Mars. Geological Society, London, Special Publications 202: 81-90. Larsen G, Guðmundsson MT, Einarsson P and Thordarson T. 2013. BÁRÐARBUNGA. In: Sólnes S, Sigmundsson F, Bessason B (eds.): Náttúruvá á Íslandi - Eldgos og /media/jar/Bardarbunga_kafli20140825.pdf

• 58. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 59. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 60. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf