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• 51. QA on the eruption in Eyjafjallajökull 2010

  There is a 24/7 watch at the IMO, where a meteorologist is present and a seismologist and hydrologist are on call. The IMO works closely with the National Emergency Agency, the University of Iceland and the British Meteorological Office, where the London VAAC (Volcanic Ash Advisory Centre) is stationed. The London office gives information on ash which are based on information from the Icelandic Met /earthquakes-and-volcanism/articles/nr/1880

• 52. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  ). The ice caps are Eyjafjallajo¨kull (ca. 81 km2), Tindfjallajo¨kull (ca. 15 km2) and Torfajo¨kull (ca. 14 km2). The DEMs were compiled using aerial photographs from 1979 to 1984, airborne Synthetic Aperture Radar (SAR) images obtained in 1998 and two image pairs from the SPOT 5 satellite’s high-resolution stereoscopic (HRS) instrument acquired in 2004. The ice-free part of the accurate DEM from 1998 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 53. ice-chart_colour-code-standard

  - 2 - Table 1. Total Concentration Colour Code Standard Colour alternative prime RGB colour model Total concentration (definition from WMO Nomenclature) Number from WMO Nomenclature 000-100-255 Ice free 4.2.8 150-200-255 Less than one tenth (open water) 4.2.6 140-255-160 1/10 - 3/10 (very open ice) 4.2.5 255-255-000 4/10 - 6/10 (open ice) 4.2.4 255-125-007 7/10 - 8/10 (close ice) 4.2.3 255 /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 54. 2010-05-02_En-IES_IMO

  of ash between 3–3.3 km a.s.l. (10,000–11,000 ft) at 60° N, 16° W (~470 km south-east of Iceland). London VAAC have been informed about this siting. Meltwater: Before 16:00 GMT, discharge levels at the old Markarfljóts bridge, ~18 km downstream from Gígjökull, were noticeably lower than yesterday's levels. Between 16:00–17:00 GMT, a meltwater pulse was detected at the bridge /media/jar/2010-05-02_En-IES_IMO.pdf

• 55. Adalgeirsdottir-etal-tc-5-961-2011

  as a ref- erence map for co-registering the SPOT5 HRS-DEM (pixel resolution of 40× 40 m), using the ice free areas surround- ing Hoffellsjökull and the correlation method described by Guðmundsson et al. (2011). This comparison revealed a hor- izontal shift of the HRS-DEM by 15 m and 5 m towards east and north, respectively, and a vertical offset of 2.3 m. Gaps in the HRS DEM, due to low contrast /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 56. Supercomputer in Iceland

  are redundant all throughout UPS (Uninterruptible Power Supply) and emergency diesel engine in place to keep infrastructure and supercomputer running even during a prolonged power outage Due to the supercomputer-friendly climate of Iceland, the potential for free cooling almost entirely eliminates the use of mechanical cooling The network Communication uses the national research networks /about-imo/news/nr/3309

• 57. Jokull-guidlines

  190-201. There are no page charges for publication in Jökull, except for colour illustrations, and authors receive a minimum of 50 reprints free of charge. Additional reprints may be ordered when galley proofs are returned to the editor. /media/jar/Jokull-guidlines.pdf

• 58. An eruption in South Iceland

  system. This description is compiled by Dr. Freysteinn Sigmundsson at the University of Iceland. The eruption is located on about 2 km wide pass of ice-free land between Eyjafjallajökull and the neighbouring Katla volcano with its overlying Mýrdalsjökull ice cap. Katla volcano is known for powerful subglacial phreatomagmatic eruptions producing basaltic tephra layers with volumes ranging from /earthquakes-and-volcanism/articles/nr/1852

• 59. The weather in Iceland 2010

  on land and in the air. The month was dry in the south and west and there was no snow on ground in Reykjavík during the first 24 days, this added to the long stretch of such days in January, to 47 consecutive snow-free days, the longest snow-free period ever observed during this time of the year. March was warm except the last five days and the first few days were very cold in the inland /about-imo/news/2011/nr/2112

• 60. The weather in Iceland 2010

  on land and in the air. The month was dry in the south and west and there was no snow on ground in Reykjavík during the first 24 days, this added to the long stretch of such days in January, to 47 consecutive snow-free days, the longest snow-free period ever observed during this time of the year. March was warm except the last five days and the first few days were very cold in the inland /about-imo/news/nr/2112