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Results:

• 71. Adalgeirsdottir-etal-tc-5-961-2011

  line shows the 2001 measured volume (57.0 km3). (B) Sensitivity to the rate factor A (in 10−15 s−1 kPa−3) and the sliding parameter C (in 10−15 m a−1 Pa−3). (C) Sensitivity to shift by one σ of ddfs and ddfi (in mmw.e.◦C−1 d−1). In (A) and (C) A= 6.8× 10−15 s−1 kPa−3, C = 0 (no sliding, method MI); in (A) and (B) ddfs = 4.0 mmw.e.◦C−1 d−1 and ddfi = 5.3 mmw.e.◦C−1 d−1; in (B) and (C) the reference /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 72. VI_2009_006_tt

  was flushed through the flood path near the end of the flood with only one-third of the flood path volume that transported a similar discharge a day or two after outflow started at the terminus. This may be interpreted as a development towards conduit flow and/or initial storage in subglacial reservoirs that do not contribute much to the transportation of flood water. Measurements of the flood water /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 73. ces_flyer_glacierssnowandice

  Climate and Energy Systems: 2007–2010 The Hydropower–Snow and Ice group http://www.vedur.is/ces Changes in glacial runoff are one of the most important consequences of ongoing and future climate change in Iceland, Greenland and some glacierised watersheds in Scandinavia. Such changes have a strong impact on the hydropower industry as discharge volumes, seasonal variations and extreme discharge /media/ces/ces_flyer_glacierssnowandice.pdf

• 74. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf

• 75. Eyjafjallajokull_SK_20101214_1

  Eldgos í Eyjafjallajökli – hlutverk Veðurstofu Íslands Sigrún Karlsdóttir, Guðrún Nína Petersen, Halldór Björnsson, Halldór Pétursson, Hróbjartur Þorsteinsson, Kristín Vogfjörð og Þórður Arason Photo: B. Pálmason Tasks of the Icelandic Meteorological Office Responsibilities: Monitoring, forecasting and issuance of warnings in the field of Meteorology Seismology and volcanic activities /media/vedurstofan/myndasafn/Eyjafjallajokull_SK_20101214_1.pdf

• 76. NONAM_participants

  @geus.dk Jes Pedersen jes.pedersen@ru.rm.dk Jórunn Harðardóttir jorunn@vedur.is Katrín Georgsdóttir kg@arborg.is Laufey B. Hannesdóttir laufeybh@lvp.is Luisa Esteban-Salvador luisaes@unizar.es Matthildur B. Stefánsdóttir matthildur.stefansdottir@vegagerdin.is Nikolai Nawri nikolai@vedur.is Ólafur Pétur Pálsson opp@hi.is Óli Grétar Blöndal Sveinsson olis@lvp.is Philippe Crochet philippe@vedur.is /media/vedurstofan/NONAM_participants.pdf

• 77. Kok_et_al._TFSC_published_2011

  l e i n f o a b s t r a c t Article history: Received 30 November 2009 Received in revised form 11 January 2011 Accepted 14 January 2011 Available online 17 February 2011 Social, natural and cultural systems are changing rapidly, influencing the future of Europe's fresh waters. One of the drivers shaping this future is the implementation of the Water Framework Directive. Participatory scenario /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 78. CES_D2_2_poster_3x3

  probability of warming, already in the next decade. Somewhat lower probability of precipitation increase, due to the relatively larger impact of natural variability. There is substantial quantitative uncertainty in climate change forecasts – do not neglect it. REFERENCES Meehl, G.A., C. Covey, T. Delworth, M. Latif, B. McAvaney, J.F.B. Mitchell, R.J. Stouffer and K.E. Taylor 2007: The WCRP /media/ces/CES_D2_2_poster_3x3.pdf

• 79. VI_2020_011_en

  ........................................................................................................................ 56 APPENDICES ......................................................................................................................... 60 A. DEM, bathymetry, and topography ............................................................................... …60 B. Input parameters used to run the mrlavaloba simulations ............................................. …61 C /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 80. VI_2022_006_extreme

  out of 11, the trend line indicates an onset of the melt season earlier in the year. For those catchments, the decrease ranges from 5 days (Hágöngulón), to 29 days (Tungnaá, see Figure 7, top panel). It should be noted that those values need careful evaluation, as the results show a great variability from one year to the other. In the case of Tungnaá, it appears that before 1995, the melt /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf