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Results:

• 1. 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

• 2. 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

• 3. Refsgaard_etal-2007-Uncertainty-EMS

  in what terms uncertainty can best be scribed. The vertical axis identifies the location or source external economic, environmental, political, social and technological circumstances that form the context of the problem.  Input uncertainty in terms of external driving forces (within or outside the control of the water manager) and system data that drive the model such as land use maps, Certainty /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 4. 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

• 5. 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

• 6. IMO's Involvement in WMO's Global Cryosphere Watch

  are the standardization of best practices, access to data, and coordination of research activities in the development of its global cryospheric observation network, called the CryoNet. Much of this development builds on existing programs and observations among a community of cryospheric scientists and organizations. Tapping into the WMO Information System (WIS) as part of WMO's Integrated Global /about-imo/news/imo-s-involvement-in-wmo-s-global-cryosphere-watch

• 7. Sea ice maps from the Norwegian Meteorological Institute

  days a week by The Norwegian Meteorological Institute, met.no, and published between 2 and 3 pm. The maps are based on satellite images. Various ice maps can be viewed on their web. The ice-map which best shows seas around Iceland is also available on our web. While viewing, it is advisable to refresh the web-site to make sure that the latest map appears. The ice chart colour code standard /sea-ice/sea-ice-maps/met-no/

• 8. CES_D2_2_poster_3x3

  of mankind) and differences between climate models (how climate responds to changes in atmospheric composition). In the short run, most of the uncertainty comes from natural variability. As shown by this example (best-estimate temperature and precipitation changes in Finland), the emission scenario uncertainty remains small until about the year 2040. Thus, during the timeframe of the CES project /media/ces/CES_D2_2_poster_3x3.pdf

• 9. Trausti_Jonsson_(IMO,_Ice)

  of large natural events in the 1960s and early 1970s showed that this line of thought was at the best wrong, but possibly also dangerous. Since then the need for natural hazard management in the broad sense has become more and more obvious in Iceland. The assessment of Icelandic natural hazards fit very well into the frame proposed by the WMO at the end of the International Decade for Natural /media/loftslag/Trausti_Jonsson_(IMO,_Ice).pdf

• 10. 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