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Results:

• 21. Demers_Claude_CES_2010

  %), households (75%) and water (90%) heating and exports ConclusionAdaptationClimate & HydrologyContext Hydro-Québec and Climate Change Extreme Climate Events Saguenay (1996 : 800 M $) Flood 1: 11,000 years checkbldThe Great Ice Storm (1998 : 1,6 Billions $)1,5 millions customers without electricity for up to 30 days Ouranos: the Mission Ouranos’ mission is to acquire and develop knowledge on climate /media/ces/Demers_Claude_CES_2010.pdf

• 22. The weather in Iceland in 2018

  In Akureyri, snow covered the ground completely for 98 days, 10 fewer than on average 1971 and 2000. The snow cover in Akureyri was heavy until mid March and number of days with complete snow cover was above average during this time. The snow conditions were light during the fall in Akureyri but a record snow depth for November (75 cm) was reached after a heavy snow fall at the end of the month /about-imo/news/the-weather-in-iceland-in-2018

• 23. CES_D2_2_poster_3x3

  FORECASTS OF CLIMATE CHANGE FOR THREE EXAMPLE LOCATIONS Probabilistic forecasts of annual mean temperature (top) and precipitation (bottom) change at three locations. The whiskers show the 2.5%, 5%, 10%, 25%, 50%, 75%, 90%, 95% and 97.5% quantiles of the probability distributions, which are given separately for the four decades 2011-2020, 2021-2030, 2031- 2040 and 2041-2050. The two numbers /media/ces/CES_D2_2_poster_3x3.pdf

• 24. Group-1_Scenarios-for-AWM

  estuary with an area of 46 km2 and mean water depth 2.9m. The catchment of Horsens has an area of 517 km2 and 75% of the area is agriculture. The area has two mean creaks, named Bygholm å and Hansted å, as well as other small streams. Coastal areas are especially vulnerable to Climate Change (IPCC, 2007). The sea level rising may bring more and more flash flood to the coastal area. The fjord /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 25. 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

• 26. Isskyrsla_20100407

  °37.30' W025°43.12' 64. N66°37.07' W025°42.88' 65. N66°35.83' W025°39.58' 66. N66°35.98' W025°38.09' 67. N66°36.72' W025°37.63' 68. N66°36.12' W025°30.75' 69. N66°40.29' W025°23.43' 70. N66°41.64' W025°22.00' 71. N66°42.18' W025°18.30' 72. N66°41.81' W025°14.49' 73. N66°43.06' W025°13.71' 74. N66°43.73' W025°15.62' 75. N66°44.26' W025°18.19' 76. N66°46.05' W025°17.16' 77. N66°45.77' W025°10.95' 78 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 27. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 28. The weather in Iceland 2013

  location t-mean dev 1961-1990 rank total dev 2003-2012 Reykjavík 4,9 0,6 36 143 -0,6 Stykkishólmur 4,4 0,9 26 168 -0,4 Bolungarvík 3,7 0,8 31 115 -0,4 Bergstaðir 3,5 -0,4 Akureyri 4,1 0,8 35 132 -0,4 Grímsstaðir 1,0 0,5 -0,6 Egilsstaðir 3,8 0,9 19 59 -0,1 Dalatangi 4,5 1,0 17 to 18 75 -0,1 Teigarhorn 4,6 0,9 /weather/articles/nr/2824

• 29. Statistical Analysis

  Journal of Physics Conference Series, Vol. 75. 8 pp. Reihan A, & Loigu E. (2007). Recent trends in water discharges of Estonian rivers. Third International Conference on Climate and Water. 3-6 September 2007, Helsinki. ISBN 978-952-11-2790-8, p.386-393. Reihan, A., Kriauciuniene, J., Koltsova, T. & Saul, M. (2010).Temporal variation of spring flood in rivers of the Baltic States In: Hydrology: From /ces/publications/nr/1943

• 30. ved-eng-2013

  of above-normal temperatures and the 15th in Akureyri in the north. location t-mean dev 1961-1990 rank total dev 2003-2012 Reykjavík 4,9 0,6 36 143 -0,6 Stykkishólmur 4,4 0,9 26 168 -0,4 Bolungarvík 3,7 0,8 31 115 -0,4 Bergstaðir 3,5 -0,4 Akureyri 4,1 0,8 35 132 -0,4 Grímsstaðir 1,0 0,5 -0,6 Egilsstaðir 3,8 0,9 19 59 -0,1 Dalatangi 4,5 1,0 17 to 18 75 -0,1 Teigarhorn 4,6 0,9 24 /media/vedurstofan/utgafa/skylduskil/ved-eng-2013.pdf