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Results:

• 1. 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

• 2. Home-page - Icelandic Meteorological Office

  /

• 3. 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

• 4. 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

• 5. 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

• 6. 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

• 7. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 8. GA_2009_91A_4_Andreassen

  /media/ces/GA_2009_91A_4_Andreassen.pdf

• 9. Journal_of_Hydrology_Veijalainen_etal

  more in Section 5.2.1. For temperature, a modification to the basic delta change meth- od proposed by Andréasson et al. (2004) was used (Eq. (1)), be- cause results from climate models indicate that cold days in Finland will warm more than the average monthly temperature (Räisänen et al., 2004; IPCC, 2007). The delta change approach therefore included a temperature-dependent component so /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 10. VI_2020_004

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