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  • 31. Monitoring device rescued from the lava

    Pedersen and Morten S. Riishuus from the Institute of Earth Sciences and Reynir Pétursson from Reykjavik Helicopters. The DOAS will be tested for any damage it may have suffered during months of being surrounded by hot lava and gases. It will be fixed and set back up near the eruption, where it will make continuous SO2 emission rate measurements that are streamed back to IMO. This instrument /about-imo/news/nr/3060
  • 32. 2010_003rs

    respectively. Several historical records of destruction resulting from earthquakes in the South Iceland lowlands exist, the oldest one from 1164 describing damage, most likely caused by an earthquake that same year (Thoroddsen, 1899 and 1905). Major sequences recur at intervals between 45 and 112 years. They often begin with a large earthquake in the easternmost part, which is then followed by a set /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
  • 33. VI_2020_008

    bridges, and culverts. This dependency necessities a new analysis of precipitation extremes and a reassessment of precipitation return periods. The modern-day availability of high temporal frequency precipitation measurements, i.e. down to 10 minutes, at various locations around the country enables testing and refinement of the original 1M5 model. Moreover, there have been major advances /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 34. 100 years of seismic observations

    in a project sponsored by the U.S. Coast and Geodetic Survey. The aim of this project was to set up an international seismic network, and in 1964 a station was installed in Akureyri as part of the World Wide Standardized Seismograph Network. From 1925 to 1964, IMO was the only institute in Iceland monitoring seismicity. In 1964, the Science Institute of the University of Iceland installed a seismograph /earthquakes-and-volcanism/conferences/jsr-2009/100_years/
  • 35. Hazard zoning

    the no-access area around the eruption site by the Icelandic Civil Protection throughout the eruption. Preliminary maps were produced considering a short meteorological data set (one month); and were only done for 50% and 90% likelihood of occurrence. A more proper data set of runs was done using 10 years of meteorological data from the ECMWF and probabilistic hazard maps accounting /pollution-and-radiation/volcanic-gas/hazard-zoning/
  • 36. Hazard zoning

    the no-access area around the eruption site by the Icelandic Civil Protection throughout the eruption. Preliminary maps were produced considering a short meteorological data set (one month); and were only done for 50% and 90% likelihood of occurrence. A more proper data set of runs was done using 10 years of meteorological data from the ECMWF and probabilistic hazard maps accounting /pollution-and-radiation/volcanic-gas/hazard-zoning
  • 37. VI_2009_012

    between three models for an Mw(v)6.5 event. .............................. 28  Figure 13. An M6.5 reference event and various PGA model predictions. ........................... 29  List of tables Table 1. Origin time, location and magnitude estimates of five calibration events. .............. 13  Table 2. Origin times and locations of the events in the data set /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 38. VI_2020_005

    is put on hazard estimation description where possible. To set the stage, emphasise the importance and motivation behind coastal flooding risk analysis and introduce the challenges of such assessments, a separate chapter that introduces different aspects of the hazard of coastal flooding, both in general and specifically in the countries of interest is presented first. There, sea levels, sea level /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 39. A FUTUREVOLC exercise

    and procedures introduced by FutureVolc. A Scientific Advisory Board was formed to discuss the evolving situation. Procedures for sending monitoring teams into the field were practiced and the set-up of new equipment for taking ash samples was tested. FutureVolc partners were able to practice evaluating monitoring data from seismometers, radar and GPS stations, the acquisition of satellite data /about-imo/news/nr/3277
  • 40. Measuring glaciers

    at the mapping of the surface of the largest glaciers using laser technology from airplane. The project is endorsed by the Icelandic Polar Year Commission. It set out in September 2008, comprising Hofsjökull, Mýrdalsjökull, Eyjafjallajökull, Eiríksjökull and Snæfellsjökull. The outlines of Icelandic glaciers have been registered, using maps, aerial photographs and satellite images. The data has been /hydrology/glaciers/

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