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  • 11. Grimsvotn_status_2011-05-30_IES_IMO

    Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf
  • 12. VI_2009_006_tt

    of the subglacial seal at the beginning of the 1996 jökulhlaup and concluded that the high water level reached before the on- set of the 1996 flood could be explained with the traditional theories of Röthlisberger (1972) and Nye (1976) but he did not address the rapid discharge increase following the breaking of the seal. Flowers et al. (2004) concluded that a model fundamentally different from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 13. VI_arsskyrsla2020

    ) in 1956. During that time that ambitions of utilizing hydropower had changed from providing the public and the sectors with electricity to aim for a large-scale utilization of hydropower for energy intensive industries. This came to fruition in 1969 with the first aluminium smelter in Iceland. Today, energy intensive industry matches fisheries as a key income sector for Icelandic society. During /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
  • 14. Hare-2011-ParticipatoryModelling

    - work. The second half of the article discusses the potential for participatory modelling to progress from being a mainly research-driven activity in the water sector to one being adopted for widespread use by water managers. By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers set up their own organizing teams, independent of researchers /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 15. Milly_etal-2008-Stationarity-dead-Science

    6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
  • 16. A heatwave in Iceland

    A heatwave in Iceland New absolute maximum temperature record in Reykjavík 31.7.2008 During the the last week of July, Iceland experienced a rare heatwave. It culminated on 30 July, when new records were set. The maximum temperature in Reykjavík /about-imo/news/nr/1362
  • 17. Strong gales

    new wind records since automatic measurements began in town in 2002. At Stórhöfði, the famous synoptic weather station located on Heimaey island's southern tip, the automatic weather station recorded wind-speed* of 44.6 m/s and gusts of 52.7 m/s, the highest since it was set up in 2004. However, that time-span is short compared to 90 years of manned observation at Stórhöfði. New records were /about-imo/news/nr/1732
  • 18. Strong gales

    and gusts measuring 45.8 m/s were recorded at the height of the storm, setting new wind records since automatic measurements began in town in 2002. At Stórhöfði, the famous synoptic weather station located on Heimaey island's southern tip, the automatic weather station recorded wind-speed* of 44.6 m/s and gusts of 52.7 m/s, the highest since it was set up in 2004. However, that time-span /about-imo/news/nr/1732/
  • 19. norsem_slunga

    Rock stress boundaries deduced from rock stress measurements Ragnar Slunga QuakeLook Stockholm AB - ragnar.slunga@quakelook.se tel.: +46703773507 Jamison and Cook (1978) analyzed the state of stress in the crust based on a set of some 50 3-D stress measurements from all over the world. They found a linear relationship between the maximum shear stress and the sum of the maximum and minimum /media/norsem/norsem_slunga.pdf
  • 20. 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

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