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• 61. Kok_and_Veldkamp_editorial_ES-2011-4160

  The American Political Science Review 97:233-243. Jessop, B. 2005. The political economy of scale and European governance. Tijdschrift voor Economische en Sociale Geografie 96:225-230. Katz, D., and I. Fischhendler. 2011. Spatial and temporal dynamics of linkage strategies in Arab- Israeli water negotiations. Political Geography 30 (1):13-24. doi:10.1016/j.polgeo.2010.12.002. Kok, K., R. Biggs, and M /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 62. Kok_JGEC658_2009

  enabling its application in domains that evolve over time. It is particularly suited for use in soft-knowledge domains with a qualitative, rather than quantitative, emphasis. The tool is said to be semi- quantitative, because the quantification of drivers and links can be interpreted in relative terms only. Axelrod (1976) introduced cognitive maps in the 1970s to represent social scientific knowl /media/loftslag/Kok_JGEC658_2009.pdf

• 63. Reykholt-abstracts

  of 2.7 km2 (20%) and a volume loss of 0.4 km³ (30%). A surface lowering of 180 m is observed near the snout decreasing to negligible amounts above 1700 m elevation. This minimal surface lowering at high altitudes is supported by a comparison of the elevation of trigonometrical points on the plateau of Öræfajökull from the Danish General Staff map of 1904 and a recent lidar-based digital elevation /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 64. VI_2020_004

  ...................................................................................... 17 2 Selected volcanoes and selected scenarios ......................................................................... 20 2.1 Hekla ......................................................................................................................... 21 2.2 Katla /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 65. Information and help

  terrain, in particular in areas where the snow cover changes from thin to thick or from hard to soft. Persistent weak layers What? Characteristics The avalanche problem is related to the presence of persistent weak layers in the old snowpack. These weak layers typically include buried surface hoar, depth hoar or faceted crystals.. Expected avalanche types Dry /avalanches/forecast/help

• 66. vanRoosmalen_etal-2009-WRR_2007WR006760

  than 1 m. [15] Groundwater abstraction varies seasonally as well as yearly owing to variable demands for irrigation. Abstraction for domestic and industrial purposes amounts to approxi- mately 10 mm/a. A model study for the area showed an average groundwater abstraction for irrigation of approxi- mately 20 mm/a [Henriksen and Sonnenborg, 2003]. How- ever, the demand for irrigation can be up to 50 mm /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 67. VI_2015_006

  6 Net downward shortwave radiation flux at the surface .................................... 18 7 Net downward longwave radiation flux at the surface ..................................... 19 8 Net downward total radiation flux at the surface............................................ 20 9 Upward sensible heat flux from the ground .................................................. 22 10 Air /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 68. VI_arsskyrsla2020

  Ísafirði og vígslu varnargarðs við Seljaland 20. október 2004. Oddur var frumkvöðull í snjóathugunum á Íslandi og byggt er á því sem eftir hann liggur í rannsóknum og bættu öryggi andspænis snjóflóðavá. Í dag starfa 20 snjóathugunarmenn víðsvegar um landið og sinna mikilvægum eftirlitsstörfum í nánu samstarfi við snjóflóðavakt Veðurstofunnar. Myndasafn Veðurstofu Íslands. Veðurstöðin á /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 69. Kok_et_al._TFSC_published_2011

  Rationale of linking exploratory scenarios and backcasts In general, both exploratory and backcasting scenarios are useful to tackle complex, wicked problems that give rise to high uncertainties on future developments while radical changes might be needed [20]. Within SCENES, it was decided that combining approaches would be benecial for a variety of reasons. Firstly, it would maximise /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 70. VI_2009_012

  Distance corrected PGV. ......................... 14  Figure 3. Corrected magnitudes, Mw(v) plotted against log distance.. .................................. 17  Figure 4. Magnitude estimates as a function of Ci. ................................................................ 18  Figure 5. Observed/predicted PGV residuals for each station. .............................................. 20  Figure 6 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf