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• 41. Bárðarbunga earthquakes 3D

  of earthquakes in Bárðarbunga 16 - 26 August 2014. IMO's specialist, Bogi B. Björnsson, compiled this video from the available data. 16 - 20 August 2014 The Bárðarbunga seismic activity can now be explored in a three dimensional video (30 sec.) which shows earthquakes from 16th to 20th August 2014. Location, depth and age of earthquakes in Bárðarbunga 16-20 August 2014. The colour /earthquakes-and-volcanism/articles/nr/2948

• 42. vhmkerfi_mars_2012

  W W W W W W W D DD DD DD CB CA CB CA CA CB CB CB CA CA CB CA CA CA CBCB CB CA CB CB CB CBCBCB CB CB CA CA CACA CA CA CACACB CA CA CA CA CB CA CA CA CA CA CB CA CA CA CACA CA CB CA CA CA CA CA CA CB CA CA CA CBCA CA CACA CA CA CA CA CA CA CA CB CA CA CA CBCB CB C CA CA CB CB CA CA CB CA CB CA CA CB CA CA CA CACA CA CB B CA CA CA CA CA CB CA CA CA CA CB CA CA CAC CACB CA CBCB CB CB CB CACA CBCA C B /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf

• 43. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/

• 44. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 45. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 46. VI_2016_006_rs

  a debris cone in the run-out zone. The source of the material is either within in the channel or in the talus slope above the channel. Most of the landslides that occur in Strandartindur are debris flows of this type. B Debris slides that are not confined to gullies and occur near a concave break of slope. The main type of material is debris mixed with fine-grained material. Most of the landslides /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 47. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 48. Updated summary from Bárðarbunga

  the migration of earthquake activity during the last days. Earthquakes in the map are colourcoded by time, dark blue dots show the onset of the swarm on Saturday, orange dots Tuesday's events until 19:00, light blue and yellow are the days in between. The time scale is days since the onset of the swarm. Map by Gunnar B. Guðmundsson, Icelandic Meteorological Office /about-imo/news/nr/2945

• 49. Aviation weather

  flight levels over Iceland and images from weather radars and satellites among other things. Simply clouds Dýrafjörður in the Westfjords, June 2008: Altocumulus lenticularis. Photo: Erna B. Antonsdóttir. Spoken weather forecast Weather information via recorded /weather/aviation/

• 50. Grimsvotn_status_2010-11-02_IES_IMO

  Grímsvötn volcano Status Report: 16:00 GMT, 2 November 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: Thorunn Skaftadottir, Egill Axelsson, Rikke Pedersen, Gunnar B. Gudmundsson and Matthew J. Roberts. Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data. Meltwater: Water continues to drain from /media/vatnafar/flod/Grimsvotn_status_2010-11-02_IES_IMO.pdf