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  • 51. raisanen_ruosteenoja_CES_D2.2

    Model Institution BCCR-BCM2.0 Bjerknes Centre for Climate Research, Norway CGCM3.1 (T47) Canadian Centre for Climate Modelling and Analysis CGCM3.1 (T63) same as previous CNRM-CM3 Météo-France CSIRO-MK3.0 CSIRO Atmospheric Research, Australia ECHAM5/MPI-OM Max Planck Institute (MPI) for Meteorology, Germany ECHO-G University of Bonn and Model & Data Group, Germany; Korean Meteorological Agency GFDL /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf
  • 52. Notes on the 2010 eruptions

    the crater, supported by lower plume (2-4 km) according to radar. MODIS satellite image shows both ash from the volcanic site and loose ash blown from the surface of Mýrdalsjökull ice cap. Comments on sound blasts, viscosity, deflation and tremors. Link to satellite image RADARSAT-2 (from the Canadian Space Agency), link to a briefing issued by WMO of frequently asked questions. 25.04.2010 – 28.05.2010 /earthquakes-and-volcanism/articles/nr/2467
  • 53. VI_2015_009

    flood models 1–24 (Eqs. 8 and 9 applied with variables 1–12). Ratio between esti- mated and reference index flood (solid black line). The solid blue line corresponds to the reference index flood (Ratio=1), estimated as the arithmetic mean of the observed AMF sample and the dashed blue lines the 95% CI derived from the GEV distribution. Large red symbol indicates overall best model. 18 4.2.2 Flood /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 54. GA_2009_91A_4_Andreassen

    (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 55. VI_2020_008

    by the Peak-over-Threshold with MLE applied on daily and 24-hour accumulated precipitation from the ICRA. ............................... 58 8 Glossary 1M5 – Daily or 24-hour precipitation return level with a 5-year return period AMSAnnual Maxima Series CCCloseness Coefficient CDOClimate Data Operator EVA – Extreme Value Analysis GP – Generalized Pareto ICRA – Icelandic /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 56. Significant ground

    commenced in December 2019. The unrest is ongoing and the occurrence of additional future earthquakes is considered likely. Click here for a larger image. Here is also a useful link on how to interpret an interferogram from our colleagues at USGS. News 2023 2022 /about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake
  • 57. Accessibility on this web site

    To improve access to the web site, the following options, among others, are available: For blind and partially sighted users, local forecasts, weather observations and seismic information can be viewed in screen readers. All the web site's text can be viewed in a screen reader. Text can be enlarged and reduced. The background colour can be changed for partially sighted or dyslexic users /about-imo/the-web/accessibility/
  • 58. Information about the conference

    for abstract submissions has been extended to 14 September. The deadline for extended abstracts is 30 October - the same day as the conference. Details about abstract submission are available via the abstract submission link. The registration fee for the conference is 5,000 ISK (30 EUR). Students can participate in the conference at the subsidised rate of 2,500 ISK (15 EUR). The registration fee /earthquakes-and-volcanism/conferences/jsr-2009/info/
  • 59. Ice subsidence above eastern Skaftá cauldron

    the subsidence did not disrupt the line-of-sight for the radio link. Ice surface lowering above eastern Skaftá cauldron 2015. This graph was updated every five minutes. These measurements are funded by FutureVolc and the research funds of the National Power Company of Iceland and of the Icelandic Road and Coastal Administration. The project is run by the Icelandic Met Office with support from /hydrology/research/skafta-cauldron/
  • 60. Ash cloud extending to Europe

    aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/nr/1873

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