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• 51. Factsheet_Bardarbunga_20141103

  site in Holuhraun. Most reliable are the forecast maps approved my meteorologist on duty, see Gas forecast. And although still being developed further, an automatic forecast, see Gas model, is also available (trial run, see disclaimer). • A new online gas detector has been put up in Hofn in Hornafjordur. Measurements of air quality can be found on the NATIONAL COMMISSIONER OF THE ICELANDIC /media/jar/Factsheet_Bardarbunga_20141103.pdf

• 52. Factsheet_Bardarbunga_20141105

  on duty, see Gas forecast. In addition there is an NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT automated model-based forecast available, this is still under development: see Gas model (trial run, see disclaimer).  A new online gas detector has been put up in Hofn in Hornafjordur. Measurements of air quality can be found on the webpage /media/jar/Factsheet_Bardarbunga_20141105.pdf

• 53. The weather in Iceland in 2019

  Mýri 451.4 103.2 83.7 44,0 173 105 Grímsstaðir 399.1 110.7 91.7 21.3 190 116 Dalatangi 1577.2 105.1 86.5 74.9 284 168 Höfn í Hornafirði 1295.0 # 81.3 45.9 219 150 Vatnsskarðshólar 1852.9 113.5 104.3 98.8 246 188 Hjarðarland 1161.3 # 91.8 64.0 /about-imo/news/the-weather-in-iceland-in-2019

• 54. Water_resources_man_Veijalainen_etal

  Volume 24, Number 13 Water Resour Manage (2010) 24:3437–3459 DOI 10.1007/s11269-010-9614-z Climate Change Impacts on Water Resources and Lake Regulation in the Vuoksi Watershed in Finland Noora Veijalainen · Tanja Dubrovin · Mika Marttunen · Bertel Vehviläinen Received: 12 July 2009 / Accepted: 22 February 2010 / Published online: 24 March 2010 ³ Springer Science+Business Media B.V. 2010 Abstract /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 55. 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

• 56. 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

• 57. Journal_of_Hydrology_Veijalainen_etal

  -dimensional hydraulic model, Two-dimensional Unsteady FLOW (TUFLOW). It uses full two-dimensional, depth averaged, momentum and conti- nuity equations for free-surface flow calculations and an alternat- ing direction implicit (ADI) finite difference method as the computational procedure (TUFLOW, 2007). The geometry data of the river channel and flood plain for the 2D hydraulic model were from /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 58. 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

• 59. 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

• 60. 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