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Results:

• 71. Climate and Modeling Scenarios

  -Skaugen, T., Haugen, J.E., & Hanssen-Bauer, I. (2008). Dynamically downscaled climate scenarios available at the Norwegian Meteorological Institute - per December 2008, met.no report 24/2008. Gregow, H. & Ruosteenoja, K. (2010). Estimating the effect of climate change on surface geostrophic winds in Northern Europe (CES Climate Modelling and Scenarios Deliverable D2.4). Finnish Meteorological /ces/publications/nr/1680

• 72. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 73. ces-oslo2010_proceedings

  ....................................... 16 CLIMATE PROJECTIONS Kjellström, E., Drews, M., Christensen, J.H., Haugen, J.E., Haakenstad, H. and Shkolnik, I. An ensemble of regional climate change scenarios for the Nordic countries........................................................ 18 Benestad, R.E. An analysis of simulated and observed storm characteristics /media/ces/ces-oslo2010_proceedings.pdf

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

  are tested: Method I (MI) that uses the same flow law parameter, A, as in the two studies discussed above, im- plicitly including basal sliding, and Method II (MII) that in- cludes a Weertman type sliding law (Paterson, 1994) where the sliding velocity is assumed to be proportional to a power of the basal shear stress, τb, (Vslid =C · τmb ); C is the slid- ing parameter and the exponent m= 3 in our /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 75. An

  /about-imo/news/an-earthquake-swarm-in-fagradalsfjall

• 76. IMO at the Arctic Circle Assembly 2017

  in sessions organised in conjunction with Arctic Circle by the World Council of Churches and the Church of Iceland on "Just Peace with the Earth", Thursday, and "Climate Justice" on Saturday. In both events he gave a presentation and took part in round table discussions. Bartholomew I patriarch of the Orthodox church also participated in the latter event.Sigrún Karlsdóttir, director of Natural Hazards /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 77. 100 years of seismic observations

  movement. The operation of the seismographs was ceased in 1914 due to funding restrictions during World War I. The operation of the seismographs was recommenced in 1925 and 1927 at the Icelandic Meteorological Office (IMO), where data processing was also conducted. Amplification of ground motion was low and even several felt earthquakes were not recorded. In 1951-1952, three Sprengnether short-period /earthquakes-and-volcanism/conferences/jsr-2009/100_years/

• 78. Increased glacial melt due to volcanic ash

  (i. e. the location of the measuring point at each river) is also available as pdf (7.2 Mb). See Jökulsá á Fjöllum in the northeast, Markarfljót in the south and Haffjarðará in the west. The volcanic eruptions in March, April and May 2010 are shown in red. Related topics /hydrology/articles/nr/2110

• 79. ces_wind_flyer-hq

  The majority of the grid cells show no significant change, however a rising trend towards the end of the century is noted (red curve). 2071 -2100 relative to 1961-90 [%] Rossby Centre i l d l Declines No change Increases Changes in % for grid cells with significant changes Activities and results reg ona mo e and ECHAM4 Rossby Centre regional model and HadAM3 ECHAM4: A2 0.1 73.2 26.7 ECHAM4: B2 0.1 /media/ces/ces_wind_flyer-hq.pdf