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• 31. Accessibility on this web site

  A text mode is available for dyslexic users. Physically handicapped users can navigate the web site without using a mouse. All link titles are clear. Images in articles include explanatory text. Attachment types are explained. A glossary is available. Instructions and explanations are available for all pages displaying real-time data. In the near future, PDF files will be available. HTML format /about-imo/the-web/accessibility/

• 32. Avalanches reported on the web

  avalanches presented on a map Jóhanna M. Thorlacius 27.4.2012 The avalanche warning service of the Icelandic Meteorological Office monitors impending avalanche danger in towns and villages in Iceland on a daily basis during the winter season. Real-time information about /avalanches/articles/nr/2477

• 33. Monitoring flow

  on an action. The data information continuously transferred to the Icelandic Meteorological Office server, can be viewed here on the website. NB: Real time data may be wrong or misinterpreted. The IMO does not take responsibility for the use of the data. Related topics /hydrology/flow/

• 34. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/

• 35. A new weather radar in the East

  alongside with such images for the South West from an older radar located next to the airport at Keflavík. Together, they cover important parts of the country with regard to volcanic eruptions. Their daily function, however, is to monitor real time precipitation. Weather radar images A weather radar reflects signals from precipitation but also from other objects it encounters, i.e. mountains /about-imo/news/nr/2528

• 36. A new weather radar in the East

  images are shown on IMO's web. Radar images from the East are now available alongside with such images for the South West from an older radar located next to the airport at Keflavík. Together, they cover important parts of the country with regard to volcanic eruptions. Their daily function, however, is to monitor real time precipitation. Weather radar images A weather radar reflects signals from /about-imo/news/nr/2528/

• 37. Articles

  Articles © Veðurstofa Íslands Averaged real time seismic amplitude (RSAM) at the seismic station on Dyngjuháls /earthquakes-and-volcanism/articles/bigimg/2970

• 38. Eyjafjallajokull_status_2010-05-21_IES_IMO

  ). Lightning: No lightning strikes have been detected since 13h, yesterday. Noises: No reports. Meltwater: Small discharge from Gígjökull. A water gauge is being installed in Kaldaklif River today. Conditions at eruption site: The eruption rate has declined a great deal and the weak plume rises from the western part of the crater. No real explosions and no lava flowing from /media/jar/Eyjafjallajokull_status_2010-05-21_IES_IMO.pdf

• 39. Economics of hazards

  policies/procedures in case of extreme weather events 9 June, 10-12 am Government Institute for Economic Research (VATT) Adriaan Perrels: Introduction - Extreme events vs. other climate change effects; economic assessment of extreme events in Finland Kevin Simmons: Effectiveness of building codes versus effectiveness of real estate markets to convey extreme event related risk information /nonam/events/nr/1930

• 40. VI_2013_006

  column. Lightning location systems, designed for weather thunderstorm monitoring are based on remote detection of electromagnetic waves from lightning and can provide valuable real- time information on location of eruption site. Important aspect of such remote detection is its independence of darkness and weather, apart from thunderstorms close to the volcano. However, the fact that individual /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf