26 results were found for 하이로미로미▥문의카톡 gttg5▥㍓하이로미로미출장椢하이마사지賙하이마사지샵䭂하이마사지업소🤸🏽‍♂️longitude/.

Results:

• 21. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 22. 2013_001_Nawri_et_al

  approximately centred around Iceland: the outer domain with 43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 95 90 grid points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The northwest corner of the outer domain covers a part of the southeast coastal region of Greenland. Otherwise, the only landmass included in the model domain /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 23. ces-oslo2010_proceedings

  Roald, L.A. and Engen-Skaugen, T. Projected effects of climate change on the hydrology of Norway ........................................................................ 80 Duncan, N.J., Harrison, G.P. and Wallace, A.R. Modelling the Scottish hydropower resource ........................................................................................................ 82 Einarsson, B /media/ces/ces-oslo2010_proceedings.pdf

• 24. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 25. VI_2013_008

  =1 day T=2 days T=3 days Statistics ME RMSE Q95–Q5 ME RMSE Q95–Q5 ME RMSE Q95–Q5 vhm 64 – method 1 6.8 48 130 13 82 215 14 101 269 vhm 64 – method 2 –2 35 97 –5.8 59 154 –9.4 84 204 vhm 64 – method 3 0.44 36 107 1.2 59 181 0.12 82 233 vhm 64 – method 4 –3.6 35 97 –6.7 57 154 –10 79 204 vhm 64 – persistence 0.03 53 / 0.02 86 / 0.05 103 / vhm 66 – method 1 1.4 15 33 1.9 21 48 1.5 23 53 vhm 66 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 26. VI_2014_006

  l l l l ll l l l l l l ll l l l l l l l l l l l l l ll l l l l l l l l ll l l l l l l l l l l ll l l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l l l l l l l l l l l l l ll l l l l ll l l l l l l l l l l l l l l l l l l l ll l l ll l l l l l −20 −10 0 10 20 − 20 − 10 0 10 Prediction (°C) R ef er en ce (° C) vhm10 Analogue (D=1) ME=−0.66RMSE=2.5 l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf