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Results:

• 51. IMO_AnnualReport2014

  is substantial since DMI is a very strong Met Institute with a strong research- and operational culture from which we have bene- fitted for a number of years. A joint forecasting area over Iceland and large part of Greenland will be one of the products of the co-operation and will improve our forecasting and warning services. The computer will be installed in our facilities which are up to the best /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

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

  point is the seminal paper by Ostrom et al. (1961), which introduced the concept of a “polycentric political system,” now more frequently referred to as polycentricity (McGinnis 2000). The basic idea is that any group of individuals facing collective problems should be able to address that problem in whatever way they best see fit. To do so, they might work through the existing system of public /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 53. GA_2009_91A_4_Andreassen

  ) and summer balance (bs) have been carried out at Storbreen since 1949. Here we apply a simple mass balance model to study the climate sensitivity and to reconstruct the mass balance series prior to 1949. The model is calibrated and validated with data from an automatic weather station (AWS) operating in the ablation zone of Storbreen since 2001. Re- gression analysis revealed that bw was best mod /media/ces/GA_2009_91A_4_Andreassen.pdf

• 54. VI_2013_008

  the feature vectors differed. The fol- lowing methods are presented: 11 - Method 1: each day, the N best analogues to current day are selected according to the shape of the MSLP fields at 12 UTC over the domain 60–70N, 35–5W (Figure 2). The analogy domain was chosen to be large enough to include areas with noticeable influence on the circulation patterns. The domain size was not strictly speaking /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 55. VI_2009_013

  the polarities available and have amplitudes within certain error limits from the measured amplitudes, are stored as possible solutions. If the relocated seismicity shows any distinct fault patterns, the joint interpretation of the events defining the fault and their mechanisms can be used to determine an overall slip direction for each fault. For each event on the fault, the mechanism best fitting /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 56. VI_2017_009

  CNRM-CM5 gives the greatest sea ice extent. According to Stroeve et al. (2012), HadGEM2 estimates the sea ice cover well and here we find it to be the second best performing model. We have now finished the selection of models and domains for the assessment of future climate in Iceland. The domain we will use is the EURO-11, the GCMs are MPI-ESM and HadGEM2, and the RCMs are COSMO-CLM and RCA4 /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 57. Paper-Olafur-Rognvaldsson_92

  - duces comparatively unbiased precipitation estimates when integrated over the Figure 7: Measured and simulated (WaSiM /MM5) mean discharge [m3s−1] at the watershed gauges. Dashed line indicates a perfect fit, solid line represents the linear best fit between the measured and simulated discharge. whole of Iceland. Table 1 compares observed and modelled discharge from six watersheds that are not much /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 58. 2010_003rs

  ........................................................ 19 2.3.2 Changing the maximum number of events in a group ................................. 20 2.3.3 Rearrange order of input .............................................................................. 22 2.3.4 Relocate only the best events ....................................................................... 22 2.3.5 Other tests /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 59. VI_2009_006_tt

  parameters used in jökulhlaup simulation. . . . . . . . . . . 63 7.2 Fitted parameters for best fit in jökulhlaup simulation. . . . . . . . . . 64 xiii xiv Chapter 1 Introduction Jökulhlaups from subglacial lakes are an important part of the hydrology of Iceland. They are most often caused by an interaction between glaciers and geothermal/volcanic activity and jökulhlaups are the most frequent hazard /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 60. Moellenkampetal_etal-2010

  for the participatory process. They also considered that he would make a decision in the best interest of the estuary and the local government, after having assessed the likely impacts of different courses of action outlined in the discussion. Impacts of the negotiation episode This negotiation episode resulted in a number of impacts apparent from evaluation data, both at the level of the co-engineering process /media/loftslag/Moellenkampetal_etal-2010.pdf