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  • 41. 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
  • 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. Observations - Gagnheiði II

    Observations - Gagnheiði II | Observations | Icelandic Meteorological office Observations - Gagnheiði II Mon 1.05 14 GMT NNE 10 Max wind : 11 / 13 13 GMT NW 5 Max wind : 5 / 10 12 GMT NW 5 Max wind : 5 / 9 11 GMT WNW 4 Max wind : 4 / 9 10 GMT NW 4 Max wind : 6 / 9 09 GMT N 6 Max wind : 6 /m/observations/areas

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