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• 31. 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

• 32. Journal_of_Hydrology_Veijalainen_etal

  precipitation and time of year (an index for available net radiation) (Vehviläinen and Huttunen, 1997). This equation has been calibrated and verified against observations of Class A pan evaporation values (Vehviläinen and Huttunen, 1997). The actual evaporation is calculated from potential evapora- tion and the soil moisture deficit. The changes in temperature and precipitation affect /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 33. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  no tcaus e mor e problem si n th e (far )futur e (20 year s o r more ) Vos s et al .( 200 6), Dub e an d Swatu k (200 2), Kicker te t al .( 199 7) Alread y no w preparation s ar e take n fo rth e (far )futur e (20 year s o r more ) Raadgeve re t al .( 200 8), Pahl-Wos te t al .( 2007 c), Vos s et al .( 200 6) 13 .Flexibl e measures , keepin g option s ope n Measure s take n no w o r propose d fo rth /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 34. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf