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

  to be always lower than 0.5 m for gentle terrain close to the ice caps for both the HRS and DMA maps and, at most, 0.6 m for the HRS maps and 1
  2 m for the DMA maps in ice- free areas of steep relief. Here, we use the highest values as a conservative empirical estimate of dh for the smooth glaciated areas (Table 2). The error in estimating the time evolution of the area (dA) in Table 2 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 12. Factsheet_Bardarbunga_20141015

  NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT THE SCIENTIFIC ADVISORY BOARD OF THE ICELANDIC CIVIL PROTECTION Date: 15.10.2014 Time: 09:30 Location: Crisis Coordination Centre, Skogarhlid. Regarding: Volcanic activity in the Bardarbunga system. Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences /media/jar/Factsheet_Bardarbunga_20141015.pdf

• 13. 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

• 14. 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

• 15. 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

• 16. ice-chart_colour-code-standard

  for ice charts only dealt with black and white charts, in keeping with the paper facsimile technology of the time, colour has long been used to help differentiate the various ice conditions on a paper chart. In the last decade, progress in computer processing and communication, as well as increased demands of users prompted the necessity to develop a new WMO International Ice Colour Code Standard /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 17. ces-glacier-scaling-memo2009-01

  but with the climate parameters corresponding to the hydro- logical year that is being considered (same climate parameters as used to calculate the mass balance in elevation-band/cell-file1). Mass balance may be specified as "NA" for ice-free ele- ments but the mass balance should be given for elements that the glacier may advance into in the next time step. Example: 6 1 0 200e6 200e6 1250 -0.7 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 18. 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

• 19. i-frame services

  The Icelandic Meteorological Office offers a service that allows web-masters to show weather information from IMO on their web-sites without effort. This service is free of charge, using the iframe technique. Two versions of iframes have been developed, one for station forecasts, text forecasts or observations, and another for weather elements (wind, temperature and precipitation forecasts /about-imo/the-web/iframes/

• 20. 47th Nordic Seismology Seminar

  and then click on "Registration" on top of that page (see screenshot). Conference costs are 30.000 ISK (~220€), to be paid upon registration. See details on cancellation policies on the registration page. Rooms at Grand Hotel Reykjavík can be booked during the registration process. Participants are free to book other potentially cheaper hotels in the vicinity.Conference costs include coffee /norsem/norsem2016/registration/