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• 41. 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

• 42. VI_2022_006_extreme

  that, the detrended timeseries would have had a net difference of zero if the negative values had not been set back to zero. This shows that over the 39 years of data, there was a slight precipitation increase for this grid-point. This trend has been removed, resulting in a detrended, almost flat dataset. 29 Figure 14. Regression lines for hourly precipitation timeseries of grid-point [100, 100] from /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 43. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 44. aerodrome_summaries_20140603

  14 0 1 2 3 8 12 15 0 1 2 3 8 12 16 0 1 2 4 8 12 17 0 1 2 4 8 12 18 0 1 2 4 8 12 19 0 1 2 4 8 13 20 0 1 2 4 8 13 21 0 2 3 5 9 13 22 1 2 3 5 9 13 23 1 2 3 4 9 13 MEAN 1 2 2 4 8 13 10 AE R OD R OM E CLIM A T OLOGICA L SUMMA R Y - T ABL E D AE R OD R OME :BIK F - KEFL A VÍ K /K efl avi k PERIO D O F RECORD :2001–201 0 L A TITUDE :6 3 59’06" N LONGITUDE :2 2 36’20" W ELE V A TIO N AB O V E MSL :5 2 /media/vedur/aerodrome_summaries_20140603.pdf

• 45. Home-page - Icelandic Meteorological Office

  /

• 46. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  ra tio n n ee ds a tho rough ,indis putable ,sci entifi c as se ss m en to ff ac ts (Fr ijte rs an d Lee ntvaa r 200 3) Th e quantit y o fdat ai sno tt he onl y issu e; dat a coll ecte d mus tals o be o fa hig h qualit y an d de pendable . 2: St at ist ic al M od el s (na tur al sy ste m ): 1: Ep ist em ic O fte n n o ts o im po rta nt M od el lin g ca pa ci ty n ee de d fo r simul atin g ef fect /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 47. Keranen_Jaana_CES_2010

  of fu tu re clim ate, hydro lo gic al m o del or wind m odel. Conse quen c e catego ry Like lih ood of th e consequ ence s to the e ne rgy pr od uc tion R isk r educ tio n / con trol / po tential D istribution netw ork P ow er p lan t En erg y sour ce, (e.g . catchme nt area , pe at or b iomass prod uctio n area ) Like lihood of th e phen om ena Sc en arios and Ph enom ena /media/ces/Keranen_Jaana_CES_2010.pdf

• 48. 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

• 49. Hare-2011-ParticipatoryModelling

  25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Fr am ew o rk Cr ite ria u se d M ain pu rp o se o fframewor k Participator y m od ell in g purpos e Particip ator y structur e Contro lo f
  ow of in for m a tio n betwee n stakeholder s Timin g of event s Participatio n mod e Mo de l typ e Participator y m et ho ds use d Actor sinvolve d (at eac h /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 50. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf