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Results:

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

  conclusions have been drawn. First, overuse, conflict, or de- struction of the resource is most likely to occur when users harvest independently or Public Choice (2010) 143: 293–301 297 are incapable of making credible commitments (Christy and Scott 1965; Anderson 1977; Libecap and Wiggins 1984; Blomquist 1992; Libecap 1995). Similarly, the experimental research investigating decision-making /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 42. VI_2015_005

  the focus is on local maxima of relative vertical vorticity. The continued use of two well-established methods for cyclone identification is due to the strengths and weaknesses inherent in both. Relative vorticity is better suited than MSLP to de- tect small-scale, fast-moving systems, such as polar lows, and is generally able to detect cyclonic storm systems at an earlier stage /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 43. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 44. Reykholt-abstracts

  Berthier3 1Institute of Earth Sciences, University of Iceland 2The Icelandic Meteorological Office 3Centre National de la Recherche Scientifique, Laboratoire d’Etudes en Géophysique et Océanographie Spatiale, Université de Toulouse, France * Corresponding author, e-mail: sg (at) hi.is ABSTRACT We assess the mass balance changes of the ~81 km2 Eyjafjallajökull ice cap in South Iceland, over three /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 45. ces-glacier-scaling-memo2009-01

  group how area changes are divided between the lowest elevation cell and higher cells. By de- fault the model adjusts the coefficient so that an estimate of the response time agrees with an estimate specified by the user in the initial glacier group file glacier-group-file0. -r rrv Relative remaining volume when to stop updating the coefficient k. When the volume of a glacier group has been /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 46. VI_2014_001

  and predicted flood quantiles were compared at gauged sites only, treated as un- gauged, for average recurrence intervals T of 2, 5, 10, 20, 50 and 100 years. The performance of the prediction was evaluated by cross-validation at independent sites not used in the method de- velopment, by calculating the mean relative error (BIAST ) and relative root mean squared error (RMSET ): BIAST (%) = 1 N N /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 47. 2010_016

  /media/ces/2010_016.pdf

• 48. 2010_017

  /media/ces/2010_017.pdf

• 49. VI_2015_006

  radiation, the net downward shortwave radiation flux at the surface varies between a minimum of 14% over snow-covered land with overcast conditions, and a maximum of 66% over the ocean with clear-sky conditions. This incoming radiation at the Earth’s surface is then converted to other forms of energy, with a distribution in percent of the net solar radiation flux, which again de- pends /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 50. VI_Arsskyrsla_2018_vef

  /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf