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• 21. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions/

• 22. Protective measures

  to the "Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Rep. 99013)" (IMO Memo TóJ-2003-05, author T. Jóhannesson) (pdf 0.03 Mb) Remarks on the design of avalanche braking mounds based on experiments in 3, 6, 9 and 34 m long chutes (IMO Int. Rep. 03024, 2003, authors T. Jóhannesson and Kr. M. Hákonardóttir) (pdf 0.8 Mb) Field observations and laboratory /avalanches/imo/protective/

• 23. Workshop on Jökulhlaup Hazards

  of over 800 inhabitants in the vicinity of the volcano. The resulting jökulhlaup drained from both the northern and southern flanks of the ice-cap, affecting an area of 57.5 and 1.5 km2, respectively. A second jökulhlaup on April 15 contained a large quantity of glacial ice; this flood propagated rapidly down the Markarfjót river, again necessitating a local evacuation. Workshop Goal The workshop /about-imo/news/nr/2251

• 24. Bardarbunga_kafli20140825

  Figure 1. The partly ice-covered Bárðarbunga volcanic system (inset, green), central volcano is indicated by capital B. Holocene lava flows from the ice-free parts of the volcanic system are shown in green, areas of thick tephra deposits are ruled. Modified after Jóhannesson and Sæmundsson (1998). No discrimination is made between lava flows of different age. In southern Iceland the area /media/jar/Bardarbunga_kafli20140825.pdf

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

  are currently melting at a fast rate. Over recent decades, annual mass balance field observations on the three largest ice caps in Iceland* Langjo¨kull (ca. 900 km2), Hofsjo¨kull (ca. 890 km2) and Vatnajo¨kull (ca. 8100 km2)*show a declining specific mass balance from about 0 m yr1 w. eq. on average from 1980 to 1994 to 1 to 1.3 m yr1 w. eq. on average after 1995 (Bjo¨rnsson et al. 2002 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 26. ice-chart_colour-code-standard

  - this is different from “No Information” which indicates that nothing at all is known about the area. 5) No specific colour is assigned to areas of “No Information”; such areas should be clearly indicated on ice charts - text annotation may be used where appropriate; an assigned colour within the code should not be used to indicate “No Information”. 6) Colour codes do not preclude use of black /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 27. Supercomputer in Iceland

  together on climate studies, Arctic studies, development and operation of the Harmonie model and other topics of mutual interest. The cooperation allows for new research opportunities, as well as further development of Nordic and International collaboration. In order to be able to accommodate the supercomputer at IMO's site, the infrastructure had to be upgraded, i.e. the uninterruptible power supply /about-imo/news/nr/3309

• 28. Jokull-guidlines

  mm and the distance between lines not less than 0.2 mm. Foldouts can only be accepted in exceptional cases. All illustrations should be identified lightly with a pencil on the back with the name of the author and the figure number. Formulae and algebraic symbols should be indicated clearly. Equations should be numbered sequentially. Numbers in brackets can refer to formulae /media/jar/Jokull-guidlines.pdf

• 29. An eruption in South Iceland

  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 dispersion model /earthquakes-and-volcanism/articles/nr/1852

• 30. Factsheet_Bardarbunga_20141015

  subsidence of the caldera occurs, causing an eruption at the edge of the caldera. Such an eruption would melt large quantities of ice, leading to a major jokulhlaup, accompanied by ash fall. Other scenarios cannot be excluded.  From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’.  From today, the Scientific Advisory Board will meet on Mondays /media/jar/Factsheet_Bardarbunga_20141015.pdf