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• 51. Ash measurements

  the National Centre for Atmospheric Science (NCAS) in the UK. The instrument transmits laser beams into the atmosphere and measures the light that is backscattered towards the ground. The instrument was installed on the lowlands close to the volcano Eyjafjallajökull which erupted last year. The aim was to measure windblown resuspended ash from last year's eruption. Following the eruption at Grimsvotn /about-imo/news/nr/2183

• 52. Flight over NW-Vatnajökull 24 Oct 2014

  Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas /earthquakes-and-volcanism/articles/nr/3008

• 53. Access_conrolled_area_20150213

  and to the south and east from those areas across the glacier. A specific hazard assessment for glacial outburst flood, jökulhlaup, in Jökulsárgljúfur is being carried out. That area is still closed to all traffic. Hazard assessment for the eruption in Holuhraun and the unrest in Bárðarbunga is under constant revision and may be changed summarily. Strict rules apply to the areas closed to traffic /media/jar/Access_conrolled_area_20150213.pdf

• 54. Eyjafjallajokull_status_2010-04-26_IES_IMO

  (~16,000 ft) between 12:00 and 14:00 GMT; elevation of 3.9 km recorded at 17:40 GMT [From aerial observations and radar measurements] Heading: Eastwards at elevations above ~4 km (~13–14,000 ft) Colour: Mostly white (steam) to the east of the crater, but grey tephra pulses above the crater Tephra fallout: No ash-fall reported, although light ash-fall possible over Mýrdalsjökull Lightening /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf

• 55. Eyjafjallajokull_status_2010-06-15_IES_IMO

  been observed at GPS stations at or around the glacier. However, a station at the northeastern caldera rim (AUST), moved about three centimeters towards the southwest from the 9th to the 13th of June, inward to the caldera. Overall assessment: The level of water in the crater lake only rose about 1 – 2 meters over the weekend. Several days or weeks are therefore likely to pass /media/jar/Eyjafjallajokull_status_2010-06-15_IES_IMO.pdf

• 56. norsem_benni

  on the basis of moment and area constraints. Thus, the model allows for consistent ground motion simulations over a large range of frequencies and distances. For simulations in the far-field region the source acceleration spectrum exists in analytical form and accounts for a high degree of earthquake source complexity and source-site geometry. In the near-fault region, the near-fault velocity /media/norsem/norsem_benni.pdf

• 57. Sea ice maps from the Norwegian Meteorological Institute

  days a week by The Norwegian Meteorological Institute, met.no, and published between 2 and 3 pm. The maps are based on satellite images. Various ice maps can be viewed on their web. The ice-map which best shows seas around Iceland is also available on our web. While viewing, it is advisable to refresh the web-site to make sure that the latest map appears. The ice chart colour code standard /sea-ice/sea-ice-maps/met-no/

• 58. Brief_report_on_gas_measurements_at_the_eruption_site_26032015

  Brief report on gas measurements at the eruption site (26 March 2015) By Baldur Bergsson and Pálmi Erlendsson General conditions: Windy day with wind coming from the west. There are still visible active fumaroles as well as heating spots across the lava field. The crater is very unstable. There are evidences of rock movements along the crater slopes since the last time the IMO team went /media/jar/Brief_report_on_gas_measurements_at_the_eruption_site_26032015.pdf

• 59. Sea ice in January 2009

  attention to the proceedings on satellite images and put information in that regard three times on the web. Easterly and northeasterly winds were dominant in the Greenland Strait. No dispatches were received from ships and the Coast Guard did not go on an exploration flight. By the end of the month sea ice maps from the Norwegian Met Office were made accessible on the IMO's web site (originally hafis /sea-ice/monthly/2009/nr/2323

• 60. Factsheet-Bardarbunga-140901

  -area. This corresponds to a magma discharge of 300 to 500 cubic metres per second. From observations yesterday evening, the volume of erupted lava is between 16 and 25 million cubic metres. The eruption has not created any ash-fall. Gas and steam rises to a couple of hundred metres above the eruption site, extending up to 1,200 m downwind. In connection with the FUTUREVOLC project, a gas /media/jar/Factsheet-Bardarbunga-140901.pdf