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• 41. Water_resources_man_Veijalainen_etal

  A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D 2010–39 (a) (b) 93. 0 93. 5 94. 0 94. 5 2040–69 Lake Pielinen 93. 0 93. 5 94. 0 94. 5 2070–99 94. 5 95. 5 96. 5 2010–39 94. 5 95. 5 96. 5 2040–69 Lake Syväri 94. 5 95. 5 96. 5 2070–99 75. 4 75. 8 76. 2 76. 6 2010–39 75. 4 75. 8 76. 2 76. 6 2040–69 Lake Saimaa 75. 4 75 /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 42. The weather in Iceland in 2022

  164 Keflavíkurflugvöllur 1081.6 98 99 41.9 226 157 The annual total precipitation in Reykjavík was 1062.4 mm, 20% above the 1991 to 2020 average precipitation. In Akureyri the total was 600.9 mm, 5% above the 1991 to 2020 mean.The number of days with precipitation equal to or exceeding 1.0 mm, were 156 in Reykjavík, 7 more than the mean 1991 to 2020 /about-imo/news/the-weather-in-iceland-in-2022

• 43. The weather in Iceland in 2020

  Skjaldþingsstaðir 1522.3 # 119 83.6 196 133 Dalatangi 1470.6 98 82 66.4 238 150 Höfn í Hornafirði 1625.2 121 104 92.9 189 134 Vatnsskarðshólar 1832.6 113 101 51.6 256 185 Hjarðarland 1395.2 # 111 70 194 164 Keflavíkurflugvöllur 1045.2 94 99 /about-imo/news/the-weather-in-iceland-in-2020

• 44. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 45. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 46. VI_2020_011_en

  Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 47. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 48. raisanen_ruosteenoja_CES_D2.2

  /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 49. vanRoosmalen_etal-2009-WRR_2007WR006760

  to the description of the geological settings in the model, such that groundwater flow can be described at high spatial resolution (horizontal discretization is 500 m and vertically 16 model layers are used). The DK model was developed for water resources assessment and planning and as 99% of the water supply in Denmark is based on groundwater, it is important that this model accurately describes /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 50. VI_2017_009

  /media/vedurstofan-utgafa-2017/VI_2017_009.pdf