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Results:

• 11. VI2010-006_web

  /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 12. VED_AnnualReport-2013_screen

  as river discharge and water levels. Notices on avalanches and sea-ice are shown; short articles and news are presented. Furthermore, web and data portals can be accessed through the web, which is available in both Icelandic and English. IMO uses the social networking website Facebook for communication and feed-back. A new web-application (App) provides access to forecasts and warnings /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 13. Climate and Modeling Scenarios

  /ces/publications/nr/1680

• 14. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  cia l sy ste m ): th re e m ai n gr ou ps o fthreat s ar e at th e scene : cl im at e, so ci o -e co n o m ic s an d gover nanc e 1: M ai nl y ep ist em ic pl us som e onto logi ca l 2:S cenari o Pa rti ci pa to ry pr oc es s (PP ) imp ortan tt o de al w ith un certaint y Pa rti cip at o ry pr o ce ss (PP )im po rta n tt o de al w ith u n ce rta in ty : Pa rti ci pa to ry go al se tti ng :c o n /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 15. IPPC-2007-ar4_syr

  warming and im- pacts than was made in the TAR. That assessment concluded that “there is high confidence2 that recent regional changes in tempera- ture have had discernible impacts on physical and biological sys- tems”. {WGII SPM} Observational evidence from all continents and most oceans shows that many natural systems are being affected by re- gional climate changes, particularly temperature /media/loftslag/IPPC-2007-ar4_syr.pdf

• 16. Adalgeirsdottir-etal-tc-5-961-2011

  images (Fig. 7 and Table 2); with an accuracy of about half the pixel size (Berthier et al., 2005). The magnitude of the SPOT5 velocity in profile DD’ is similar to the observations made in the 1930s (Fig. 6a). A good spatial coverage was obtained by using two SPOT im- ages from late summer 2002, but reliable signals were only obtained for limited areas when an attempt was made to de- termine /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 17. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  e in relatio n to climat echang eadapt ation .X ,X X ,XX X is a ge n era lguid eo n th e relativ e imp ortanc e leve lo fth e sourc es , alth oug h it mus tb e em phasise d tha tth e imp ortanc e o fth e indi vidua lsou rce s o fun certaint y is co n tex tspe cifi c St ep si n cl im at e ch an ge ad ap tat io n an al ys es (ch ain in u n ce rta in ty ca sc ad e, Fi g. 2) So ur ce s o fu n ce rta /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 18. Statistical Analysis

  /ces/publications/nr/1943

• 19. 2005EO260001

  im- proved by a double-difference location meth- od [Slunga et al., 1995], and supported by P - wave particle-motion analysis at GRF, reveal a northerly trending event distribution, centered at the southern caldera rim, ~1 km east of the main eruption site (Figure 1b). Focal depths mostly concentrate above 4 km and decrease by ~2 km near the eruption onset. The detection threshold /media/jar/myndsafn/2005EO260001.pdf

• 20. Hare-2011-ParticipatoryModelling

  Simulatio n mode l (scientific ) Im pr o ve m o de l (quality ) Fa rm er s, Fa rm busines s advisor sNO P IN D Interview s NO P IN D Qu es tio n n ai re – verificatio n NO P OT :Researcher s M KA/ M M (re nements ) KA M Has e I Simulatio n mode l (scientific ; discussio n su pp o rt ) Im pr o ve m o de l (quality , acceptance ) Farmers ,loca l authorities , association s IN D Reques t fo rdat a N /media/loftslag/Hare-2011-ParticipatoryModelling.pdf