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  • 81. Johannesson_Thomas_CES_2010

    of Time- Variable Gravity Show Mass Loss in Antarctica. Science, 311, 5768, 1754 – 1756. DOI: 10.1126/science.1123785. Wouters, B., D., Chambers and E. J. O. Schrama. 2008. GRACE observes small-scale mass loss in Greenland. Geophys. Res. Lett., 35, L20501, doi:10.1029/2008GL034816. Meier, F. M., and others. 2007. Glaciers Dominate Eustatic Sea-Level Rise in the 21st Century. Science, 317, 1064–1067 /media/ces/Johannesson_Thomas_CES_2010.pdf
  • 82. Journal_of_Hydrology_Veijalainen_etal

    in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 83. Guidelines2-for-rapporteurs

    o n 4 . 1 X s e s s i o n 4 . 2 X s e s s i o n 4 . 3 X s e s s i o n 4 . 4 X s e s s i o n 4 . 5 X F r i d a y 3 1 . 8 p l e n a r y 4 X s e s s i o n 5 . 1 X s e s s i o n 5 . 2 Xsession 5.3 X sess on 5.4 X session 5.5 X lunch plenary panel 2 X TOTAL TURNS PER PERSON 2 2 2 2 2 2 3 2 3 2 3 2 3 2 /media/loftslag/Guidelines2-for-rapporteurs.pdf
  • 84. VI_2014_005

    and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 85. ces-glacier-scaling-memo2009-01

    in Norway was provided by the Norwegian Water Resources and Energy Directorate (NVE). TóJ 12 5.12.2009 Memo References Bahr, D. B., M. F. Meier and S. D. Peckham. 1997. The physical basis of glacier volume–area scaling. J. Geophys. Res., 102(B9), 20,355–20,362. Björnsson, H., and F. Pálsson. 2008. Icelandic glaciers. Jökull, 58, 365–386. Fenger, J. (Ed.). 2007. Impacts of Climate Change on Renewable /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 86. VI_2014_006

    and candidate situations is evaluated with the Teweles-Wobus (S1) skill score (Wilks, 1995). The S1 score compares the shape of two fields by considering their gradient at each grid point of the analogy domain: S1(u) = 100 n 1 i=1 m j=1 jDAi DFij+ n i=1 m 1 j=1 jDA j DFjj n 1i=1 m j=1 Gi + n i=1 m 1 j=1 G j (3) with DAi = A(i+1; j;u) A(i; j;u) (4) DFi = F(i+1; j; t) F(i; j; t) (5) DA j /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
  • 87. 2010_016

  • 88. VI_2009_013

    Th. Árnadóttir, C. Völksen, W. Jiang, E. Sturkell, T. Villemin, P. Einarsson, F. Sigmundsson, and R. Stefánsson (2006). Current plate movements across the Mid- Atlantic Ridge determined from 5 years of continuous GPS measurements in Iceland. J. Geophys. Res., 111, B09407, doi:10.1029/2005JB003717. Guðmundsson, Á., S. Brynjólfsson (1993). Overlapping rift zone segments and the evolution /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
  • 89. VI_2015_006

    longwave radiation and latent heat losses, and small downward sensible heat fluxes. This excess energy then becomes available for melting of surface snow. The energy needed to melt a given mass of snow, ms, is given by E = ms L f ; (1) where L f = 334;000 J kg 1 is the latent heat of fusion. With an hourly change in snow water equivalent due to melting, dDmelt, the amount of energy absorbed /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 90. askja_minnisblad_ens

    the next years, decades or centuries. Consequently, travel near the lake is associated with a certain risk. A person by the lake that notices a landslide should move immediately up the hill and away from the lake. It takes a tsunami wave about 1–2 minutes to travel across the lake and sound takes about 10 sec to cover that distance. Thus, people have a very short time to escape if a big /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

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