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• 51. Hazard zoning

  for seasonal variability have been produced. The CALPUFF model has been initialized with SO2 flux data as coming from the DOAS monitoring system (Gislason et al., 2015). Maps based on ten years of meteorological data Each map below shows the likelihood that at a specific location the hourly ground concentration of SO2 will exceed a specific threshold. The threshold values are shown in bold blue /pollution-and-radiation/volcanic-gas/hazard-zoning

• 52. ces_geus_paakitsoq_full_report

  offsets between measurements and downscaled RCM fields at Crawford and Swiss Camp (1995-2006) are calculated. The offset-values are averaged over both stations and all years to obtain a correction value for each day of the year. Due 9 Figure 8: Mean annual accumulation distribution for the Paakitsôq area according to RCAO (Plot a) and HIRHAM4 (Plot b). to time constraints it was decided to calculate /media/ces/ces_geus_paakitsoq_full_report.pdf

• 53. A new ice-cauldron in Öræfajökull volcano

  the area with scientists tomorrow to collect additional data and samples. The Icelandic Meteorological Office has increased the surveillance of the area and is monitoring the volcano closely in collaboration with scientists from the University of Iceland and the Icelandic Civil Protection Authorities. The Icelandic Meteorological Office has in light of this elevated activity raised the aviation /about-imo/news/a-new-ice-cauldron-in-oraefajokull-volcano

• 54. Bardarbunga_Daily_status_report_230814

  Bárðarbunga update 23082014 2014-08-23 15:00 UTC Bárðarbunga update Compiled by Melissa Anne Pfeffer Sara Barsotti Hildur María Friðriksdóttir Kristín Jónsdóttir Kristín Vogfjörð Bergur Einarsson Benedikt G. Ófeigsson Þóra Árnadóttir Ásta Rut Hjartardóttir Michelle Parks Based on Seismic, GPS, water samples Eruption plume Height (a.s.l.) Subglacial eruption, no eruption cloud. Heading Subglacial /media/jar/Bardarbunga_Daily_status_report_230814.pdf

• 55. Mo_Birger_CES_2010

  Quantitative system analysis 18 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Average annual characteristics for the NordPool area 0 9 18 27 36 45 52 0 0:2 0:4 0:6 0:8 1 105 Week GW h Reservoir level Reference Echam Hadam 0 9 18 27 36 45 52 0 0:2 0:4 0:6 0:8 1 1:2 1:4 104 Week GW h In ow 0 9 18 27 36 45 52 2;500 3;000 3;500 4;000 4;500 5;000 5;500 Week GW /media/ces/Mo_Birger_CES_2010.pdf

• 56. HARMONIE - numerical weather prediction model 

  was originally suggested by Páll Bergþórsson, former director of IMO, and Bo R. Döös in 1955. In addition to the analysis, the model also needs prediction of the development of weather at the boundaries of the domain, retrieved from a coarser resolution global NWP simulation from the European Centre for Medium-Range Weather Forecasts (ECMWF). HARMONIE is developed for horizontal resolution ranging from /weather/articles/nr/3232

• 57. Avalanche dams

  ofan byggðarinnar. (Náttúrufræðingurinn, 69, 1, 3−10, 1999, authors T. Jóhannesson, O. Pétursson, J. G. Egilsson and G. G. Tómassson) [abstract] (html) A map on a selected front page shows recent observations of avalanches. For user access to avalanche and landslide data, an avalanche map viewer is available /avalanches/imo/dams/

• 58. VI_2009_012

  = b·Mwi CMT + c , i = 1,…5, with b = 1 and the parameter c estimated by least squares to be -4.88. Having determined c, the magnitudes of all earthquakes in the data set are recalculated according to: Mw(v)i := Ci + 4.88 With a determined to be -1.63 in the first step, the resulting log-linear attenuation relationship becomes: 88.4)(log63.1)(log 1010 −+⋅−= MrPGV , (A) Equation /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 59. ces_cg_flyer

  and regional models all under the IPCCA1B emission scenario (right) have been accomplished, see http://ensemblesrt3.dmi.dk Relative changes comparing 2021-2050 to 1961-1990 in three of the CES RCMs are shown for annual mean precipitation (above) and 10m-wind speed (below). Units: %. Partners The work in the Climate modelling and scenarios group is carried out by a network of scientists from the national /media/ces/ces_cg_flyer.pdf

• 60. Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik

  Impacts of Climate Change on Stormwater Systems in Reykjavík Ásta Ósk Hlöðversdóttir1*, Philippe Crochet2, Jónas Elíasson1, Hrund Ó. Andradóttir1 and Brynjólfur Björnsson3 1 University of Iceland, 2 Icelandic Meteorological Office, 3 Mannvit Engineering *Corresponding author. Email address: aoh3@hi.is Due to climate change, precipitation is projected to increase in Northern Europe (Bates /media/loftslag/Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik.pdf