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Results:

• 11. Avalanche bulletin - Northern Westfjords

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• 12. Avalanche bulletin - Southwest corner

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• 13. Benestad_Rasmus_CES_2010

  An analysis of simulated and observed storm characteristics - Can we expect a change in the future? R.E. Benestad, CES, June 01 2010 Number of cyclones: RCM analysis CCI (Benestad & Chen, 2006) righttoleftmark No change in storm frequency? RCM: N corresponds |v| too high ...or simulated wind speeds? •CCI •triangulation Method: storm characteristics RCM: storms too small too strong. Gradient /media/ces/Benestad_Rasmus_CES_2010.pdf

• 14. 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

• 15. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 16. Avalanche bulletin - Eyjafjörður (experimental)

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• 17. Avalanche bulletin - Tröllaskagi

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• 18. Avalanche bulletin - Eyjafjörður (experimental)

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• 19. Avalanche bulletin - Tröllaskagi

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• 20. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf