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Results:

• 31. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 32. Milly_etal-2008-Stationarity-dead-Science

  Nature 438, 303 (2005). 8. J. Lu, G. A. Vecchi, T. Reichler, Geophys. Res. Lett. 34, L06805 (2007). 9. S. Manabe, R. J. Stouffer, J. Geophys. Res. 85, 5529 (1980). 10. P. S. Eagleson, in Scientific Basis of Water-Resource Management (National Academy Press, Washington, DC, 1982). 11. N. C. Matalas, in Global Change and Water Resources Management (Water Resources Update No. 112, Universities /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 33. 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

• 34. 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

• 35. 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

• 36. vonKorff_etal-2010

  /media/loftslag/vonKorff_etal-2010.pdf

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

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 38. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 39. VI_2009_012

  The medians of ratios from the broad-band digitizers (G24) are close to one, but the lowest median values are obtained at stations with short-period digitizers (RD3) in combination with either 1-Hz short-period (LE1) sensors, or broad-band (BB) sensors. The reason for the low ratios in the LE1-RD3 combination is obviously failure to retrieve all the low frequency amplitude through instrument /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 40. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf