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  • 71. High resolution precipitation maps for Iceland

    maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625
  • 72. Hock_Regine_CES_2010rs

    Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf
  • 73. norsem_lindholm

    Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf
  • 74. VI2010-006_web

    5.6 Hafnarstræti 23–89 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 5.7 Grófargil . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36 5.8 Gleráreyrar og farvegur Brunnár . . . . . . . . . . . . . . . . . . . . . . . . . 36 6 Niðurstaða 37 7 Heimildir 38 Viðaukar I Tæknileg hugtök og skilgreiningar 41 II Langsnið brauta 43 III Kort 49 5 6 1 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
  • 75. VI_2015_009

    .............................................................. 19 5 Conclusion .................................................................................................. 23 6 Acknowledgements....................................................................................... 23 7 References .................................................................................................. 24 Appendix I - Identification /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 76. VI_Arsskyrsla_2018_vef

    grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
  • 77. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

    mover’s payoff, while mover 2’s payoff is greater than or equal to the first mover’s payoff. The payoff function is that of the basic public good game. The marginal return from the public good is a ∈ [0,1], and each agent’s initial endowment is E. The payoff function Rik of agent i as mover k, k = 1 for the first mover and k = 2 for the second mover, is defined as follows: Rik =E − xik + a (xik /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
  • 78. IMO receives Special Achievement Award for Exceptional Application of Geospatial

    to improve our world," says Esri president Jack Dangermond. "Each year I look forward to being part of this ceremony. It is a tradition that means a great deal to Esri and to GIS professionals." More information is available about the 2011 Special Achievement in GIS Award winners, including project information and photos. There, examples of IMO's work can be seen /about-imo/news/nr/2241
  • 79. norsem_atakan_ip

    and sustainable society. The main vision of the European Plate Observing System (EPOS) is to address the three basic challenges in Earth Sciences: (i) unravelling the Earth's deformational processes which are part of the Earth system evolution in time, (ii) understanding the geo-hazards and their implications to society, and (iii) contributing to the safe and sustainable use of geo-resources /media/norsem/norsem_atakan_ip.pdf

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