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  • 81. VI_2019_009

    a71 a71 a71 a71 a71 a71 a71 a71 0 10 20 21 23 24 30 51 52 53 61 62 64 67 71 72 73 81 85 87 1 2 3 10 11 14 15 16 20 21 22 23 25 26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 a71 5 10 15 20 5 10 15 20 Number of records Figure 16. Automatic records as a function of manual /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 82. VI_2015_007

    0.95 vhm149 1.46 vhm205 1.01 vhm206 1.28 vhm221 0.9 vhm265 1.16 vhm277 0.87 vhm278 -0.12 18 l l l l l llll l llll lll ll lll lllll lllll ll l l l l l l l l l l l −2 0 2 4 6 0 1 2 3 4 −ln(−ln(1−1/T)) Q/ E[ Q] 1 2 5 10 20 50 100 T (years) l l l l l l l l vhm148 vhm149 vhm205 vhm206 vhm221 vhm265 vhm277 vhm278 Regional +/− 95% CI H1 0.995 H2 −0.877 l l l l l l l l l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
  • 83. Journal_of_Hydrology_Veijalainen_etal

    emission scenario were even greater, on average 5.1% units (Fig. 5), indicating that the GCMs are a greater source of uncertainty than the choice of emission sce- nario or RCM. The flow regimes in different regions in Finland are demon- strated with the five example hydrographs of the reference period and of 2070–2099 (Fig. 8a–e, see Fig. 1c for locations). In northern (Fig. 8a) and central (Fig. 8b /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 84. VI_2014_006

    scale, used to identify weather analogues. These fields are extracted twice daily (00UTC and 12UTC) on a 1 x 1 latitude-longitude grid from the ECMWF operational analysis and forecasts available for the period 2001–2006. The ana- logue meteorological situations are extracted from the ERA-40 reanalysis archive (Uppala et al., 2005) for the period 1958–2001. 14 Predictants: Gridded series of daily /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

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