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• 71. Isskyrsla_20100120

  :00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 Samtals########### ########### 720 Flugleið:BIRK Garðskagi fyrir jökul og norður um fyrir Vestfirði. Farið dýpra til baka, um Víkurál og Skerjadýpi. Flugskýrsla TF-SIF Dags 20.01.2010. Flug nr. 00410.025 Ísdreifar sáust á ratsjá norður af Horni, þó ekkert sem hægt er að kalla samfellt. Ísröndin var næst landi 50 sml. NV frá Straumnesi /media/hafis/skyrslur_lhg/Isskyrsla_20100120.pdf

• 72. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 73. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 74. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 75. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 76. Öræfajökull : Recent research

  of the chapters can be downloaded or short summaries read.Downloadable material:Full text (pdf 23 Mb)Front matter (pdf 180 Kb)Table of contents (pdf 7.9 Kb)Chapter I. Volcanogenic floods in Iceland: An exploration of hazards and risks (pdf 1.06 Mb)Pages 7–16Emmanuel Pagneux, Sigrún Karlsdóttir, Magnús T. Gudmundsson, Matthew J. Roberts og Víðir ReynissonShort summaryChapter II. Öræfajökull Volcano /volcanoes/about-volcanoes/oraefajokull/new-research/

• 77. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf