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• 11. 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

• 12. 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

• 13. VI_2009_006_tt

  flow . . . . . . . . . . . . . . . . . . . . . 30 4.6 Water flow in jökulhlaups . . . . . . . . . . . . . . . . . . . . . . . . 30 5 Data 33 5.1 Discharge in Skaftá and the September 2006 jökulhlaup . . . . . . . . 33 5.2 Discharge from the cauldron . . . . . . . . . . . . . . . . . . . . . . 36 5.3 Temperature measurements . . . . . . . . . . . . . . . . . . . . . . . 44 6 Results and interpretation /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 14. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 15. norsem_voss

  Geological Survey of Denmark and Greenland – GEUS Peter H. Voss GEUS The goal for the seismic service at GEUS is simply; to monitor and register earthquakes and other seismic activity including possible nuclear explosions. For this purpose GEUS maintains an earthquake database covering registered seismic activity in the Kingdom of Denmark. Both the resources for and the quality /media/norsem/norsem_voss.pdf

• 16. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 17. VI_2017_009

  domain in the eight main cases. The periods calculated are the entire 21st century (2000–2100), the mid- century (2041–2060), and the late-century (2081–2100). For explanation of these cases see Table 3. Case GCM,RCM,RCP Mid-century Late-century Entire 21st century 1 HAD,RCA4,45 .28 .27 .29 3 HAD,COSMO,45 .26 .25 .26 5 MPI,RCA4,45 .24 .16 .26 7 MPI,COSMO,45 .22 .15 .21 2 HAD,RCA4,85 .33 .41 /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 18. Session program Wednesday 12. October

  in the Kingdom of Danmark - challenges and future development Peter H. Voss 11:30 – 11:50 The ISC data (and how to get it) James Harris, Dmitry Storchak11:50 – 13:30 Lunch break13:30 – 15:10 Oral session - Chair: Annakaisa Korja 13:30 – 13:50 Neotectonics in Nordland; NEONOR 2 Conrad /norsem/norsem2016/program/wednesday

• 19. Demers_Claude_CES_2010

  and barriers to adaptation • Conclusions Presentation outline 60 checkbld 10 % of the Québec territory, 1,600,000 km² checkbld 4,500 rivers checkbld 500,000 lakes checkbldcheckbld checkbldcheckbld checkbldcheckbld Québec hydrography 2,000 km 60 Hydro plants / 34,499 MW / 188 TWh 2009 #1 Hydro 42 run-of-the-river / 18 with reservoir Power houses 175 TWh storage capacity La Grande River Hydro Project /media/ces/Demers_Claude_CES_2010.pdf

• 20. 2010_005_

  in hectopascals during the 1961–90 control period, for the reanalyses and the RCMs. . . . . . . . . . . . . . . . . . . 32 11 Dependence on terrain elevation of linear trends of total precipitation within the 2004–50 period in the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5, together with the corresponding model orographies. . . . . . . . . . . . . . . . . . 33 6 12 Mean annual total precipitation /media/ces/2010_005_.pdf