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  • 71. Bárðarbunga 2014 - November events

    moment is presented as well. These images were made at 26 Nov at 14:21. 28 November 2014 11:30 - from the Scientific Advisory Board Scientists flew over Bárðarbunga on Wednesday, 26 November. According to data acquired in the flight, the total subsidence of the caldera is 50 meters and the volume is 1.4 cubic kilometers. No signal is now received from the station in the caldera /earthquakes-and-volcanism/articles/nr/3023/
  • 72. Mission

    % with Ph.D. degree. The gender balance of the office is 65% male and 35% female.The main purpose of IMO is to contribute towards increased safety and efficiency in society by: Monitoring, analyzing, interpreting, informing, giving advice and counsel, providing warnings and forecasts and, where possible, predicting natural processes and natural hazards;issuing public and aviation alerts /about-imo/mission/
  • 73. Lava flows

    23 72 792 18 Hallmundarhraun 950 Pahoehoe lava 33 55 255 8 Skaftáreldahraun 1783-1784 Pahoehoe lava 25 65 599 14 Gjástykki; Krafla eruption 1980. Photo: Oddur Sigurðsson /volcanoes/volcanic-hazards/lava-flow/
  • 74. norsem_ingi

  • 75. IMO_AnnualReport2014

    a dust cloud created by the rockslide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a “rotational slide movement”, which means that the failure surface of the slide is con- cave. The volume of the slide is roughly estimated 30–50 million m³, however, the estimation may change when further /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 76. VI_arsskyrsla2020

    og dreifingu gjósku í eldgosum. Í kjölfar Eyjaallajökulsgossins 2010 bættist önnur við á Austurlandi og síðan tvær færanlegar, sérstaklega til þess að vakta eldgosavá. Mynda- safn Veðurstofu Íslands. 20 ÁRSSKÝRSLA 2019 Brúarfoss. Ljósmynd: Einar Guðmann. 21 „TÍMI OG BREYTILEIKI Í VATNAFRÆÐI“ Í tilefni af 50 ára afmæli Vatnamælinga 1997 „Í dag stöndum við andspænis þeirri staðreynd, að /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
  • 77. VI_2014_005

    coordinate system, where model levels are defined as iso-surfaces of pressure, scaled by the pressure at the lower model boundary. For IMO reanal- yses, the model is run with the standard 65 vertical levels, and with a non-hydrostatic dynamic core (DYNAMICS=“nh”). Radiation, turbulence, convection, and microphysics (clouds and pre- cipitation) are determined by the AROME upper air physics scheme /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 78. raisanen_ruosteenoja_CES_D2.2

    changes are expected to have a 50% probability of occurrence. Figure 3.1. Best estimates of temperature change. The top row represents temperature changes for the decade 2011-2020 in four three-month seasons (winter = December-January-February; spring = March-April-May; summer = June-July-August; autumn = September-October-November). The bottom row shows the best estimates of annual mean temperature /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf
  • 79. snz_kort_idk

    ïï A A A A AA A A A A Markarfljót Farið Hvítá við Kljáfoss Hvítá við Fremstaver Austari Jökulsá Jökulsá á Fjöllum Skaftá Haffjarðará Hvítárvatn Þjórsá við Norðlingaöldu scale 1: 1.850.000 Cartography: Meteorological Office/IDKProjection: Keiluvörpun Lamberts. Datum: ISN93Base map: Landmælingar Íslands Vatnajökull Langjökull Mýrdalsjökull Hofsjökull 0 50 10025 km ¨ Legend ï volcanic eruption 2010 /media/vatnafar/flod/snz_kort_idk.pdf
  • 80. 2010_012rs

    .......................................................................65 6 SAFER Rannsóknaverkefnið Í Evrópusamstarfsverkefninu SAFER (Seismic eArly warning For EuRope) var unnið að rannsóknum og þróun á rauntímaúrvinnslu jarðskjálftabylgna um leið og þær berast í mælistöðvar í því markmiði að þróa ferla sem geta nýst til viðvarana og viðbragða áður en stærstu og skæðustu jarðskjálftabylgjurnar berast til viðkvæmra mannvirkja eða /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

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