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• 51. 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

• 52. 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

• 53. Factsheet_Bardarbunga_20141015

  Air quality:  Today (Wednesday) light easterly winds are expected. The gas pollution that has been hovering over the country as well as the gas erupted today will move slowly towards the west. The eastern part of Iceland will therefore be pollution free in the afternoon, but in most other parts of Iceland, pollution can be expected, and air quality can be poor in places. Tomorrow (Thursday /media/jar/Factsheet_Bardarbunga_20141015.pdf

• 54. 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

• 55. 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

• 56. ved-eng-2010

  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. A fissure volcanic eruption started at Fimmvörðuháls on the 20th. The temperature in April was close to the average. There was much snow disrupting traffic in the northeast during /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 57. QA on the eruption in Eyjafjallajökull 2010

  amount of ice is melted and, accordingly, little danger of large jökulhlaups. The floods are monitored by online gauges in several rivers around the volcanoes Katla and Eyjafjallajökull. Large or damaging jökulhlaups are not expected in connection to this event unless changes occur in the eruption pattern. How is the eruption monitored? The Icelandic Meteorological Office monitors earth /earthquakes-and-volcanism/articles/nr/1880

• 58. ces-glacier-scaling-memo2009-01

  of the area and mean elevation for the ice-free and glaciated parts of each elevation band or grid cell. The areas are denoted by ai and gi, and the elevations by zi and yi, for the ice-free and the ice-covered areas, respectively. At the end of each hydrological year, the hydrological model will provide a simulated value for the total mass balance of each glacier group within the watershed, DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 59. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 60. Hydropower - Glacier, Snow and Ice

  of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.). Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1. Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I /ces/publications/nr/1940