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  • 21. ces-oslo2010_proceedings

    and future precipitation in the Baltic Sea region as simulated in a suite of regional climate models. Climatic Change 81, 281-291. Nakićenović, N., and R. Swart (eds.), 2000. Special Report on Emissions Scenarios. A Special Report of Working Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 599 pp. van der /media/ces/ces-oslo2010_proceedings.pdf
  • 22. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  • 23. Group-1_Scenarios-for-AWM

    and Vulnerability, Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Jaroslav Mysiak, Hans Jørgen Henrikson, Caroline Sullivan, John Bromley and Claudia Pahl-Wostl, 2010, The Adaptive Water Resource Management Handbook, Earthscan Dunstan House, pp 199. /media/loftslag/Group-1_Scenarios-for-AWM.pdf
  • 24. About the implementation

    are in the forefront. Architecture It was decided to use the Eplica content management system. It is as a Java based system so specific dynamic components were written in Java. It was decided to use Servlets and the MVC pattern, with minimal usage of Eplica API. This way the components may be moved and reused with minimal efforts in other Java CMS or converted to Portlets (JSR 168) if and when /about-imo/the-web/implementation/
  • 25. VI_2015_005

  • 26. vanRoosmalen_etal-2009-WRR_2007WR006760

    to a maximum of 1.15 on day 75, after which Kc reduces to 1.05 at harvest time. After the growing season the grain area is assumed to be represented by bare soil for the winter season. [33] The other land use types have constant parameters throughout the year, except for LAI values for grass, which increase from 2.2 on 1 April to 4.5 in approximately 60 days, when the grass is cut and the LAI value /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 27. Publications 2009

    in the Eyjafjallajökull volcano Sigurlaug Hjaltadóttir, Kristín Vogfjörð & Ragnar Slunga 33 pp 3,2 Mb 2009-012 Attenuation relations for near- and farfield peak ground motion (PGV, PGA) and new magnitude estimates for large earthquakes in SW-Iceland Gunnar Geir Pétursson & Kristín S. Vogfjörð 43 pp 1,9 Mb 2009-006 Jökulhlaups in Skaftá: A study of a jökulhlaup from the western /about-imo/publications/2009/
  • 28. 16910025

    BIRK 12:01 12:04 03:26 03:33 820 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 Samtals 03:26 03:33 820 Flugleið: Flugskýrsla TF-SIF 30. nóvember 2010 Flug nr. 16910.025 Texti: Kl.0941, skipaumferð á NA- og A- landi. Kl.0948, kallað í Havfrakt OZ2056 á ch-16. Hann er að koma frá Þórshöfn í Færeyjum og er á leið til Þórshafnar á Langanesi /media/hafis/skyrslur_lhg/16910025.pdf
  • 29. CES_D2.4_VMGO

    L. Michaelis, S. Mori, T. Morita, W.Pepper, H. Pitcher, L. Price, K. Raihi, A. Roehrl, H.-H. Rogner, A. Sankovski, M.Schlesinger, P.Shukla, S. Smith, R. Swart, S. van Rooijen, N. Victor, Z. Dadi, 2000: IPCC Special Report on Emission Scenarios. Cambridge University Press, United Kingdom and New York, NY, USA. a) b) c) Fig.1 Change of annual extreme temperature range /media/ces/CES_D2.4_VMGO.pdf
  • 30. The weather in Iceland in 2021

    56.2 180 136 Vatnsskarðshólar 1507.3 87 81 61.9 259 188 Hjarðarland 1415.2 106 108 66.5 201 160 Keflavíkurflugvöllur 1071.3 97 98 38.2 241 171 Table 2: Precipitation overview 2021 from several stations. (1) Total precipitation (mm). (2) Percentage of the 1991 to 2020 average precipitation. (3 /about-imo/news/the-weather-in-iceland-in-2021

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