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21. Other institutions

Space Agency ESA National/Naval Ice Center's website The Cryosphere Today - University of Illinois National Snow and Ice Data Center - NSIDC Polar Data Catalogue - Canadian Cryospheric Information Network Related content /sea-ice/webs/

22. Technical problem solved

7.9.2012 Technicians have done a certain repair work for IMO‘s data bases which are now receiving information and observations as usual. The presentation should be back to normal, both for weather forecasts and other data. Full interaction is, however, not guaranteed and our /about-imo/news/nr/2526

23. VI_2021_008

off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

24. Staff members

25. Staff members

26. Staff members

27. Monitoring flow

floods originating in sub-glacial volcano and geothermal systems, or melt water, heavy rain and ice blockage of river-flow. The development of the network began in 1996, following jökulhlaup in Skeiðará, and has in the last decade been extended to the areas south and north of Vatnajökull, south of Mýrdalsjökull, the South Iceland lowland and to Borgarfjörður. Each monitoring station has /hydrology/flow/

28. norsem_lund

more events in the vicinity in the next two months. These aftershocks are interesting as aftershocks to M4+ events are not always observed in Sweden and Finland. The Bothnian Bay is one of the most seismically active areas in continental Fennoscandia, but the cause of the seismicity is still not well known. Until recently, the offshore areas have been poorly monitored by the national seismic /media/norsem/norsem_lund.pdf

29. Hazard zoning

for seasonal variability have been produced. The CALPUFF model has been initialized with SO2 flux data as coming from the DOAS monitoring system (Gislason et al., 2015). Maps based on ten years of meteorological data Each map below shows the likelihood that at a specific location the hourly ground concentration of SO2 will exceed a specific threshold. The threshold values are shown in bold blue /pollution-and-radiation/volcanic-gas/hazard-zoning/

30. Hazard zoning

for seasonal variability have been produced. The CALPUFF model has been initialized with SO2 flux data as coming from the DOAS monitoring system (Gislason et al., 2015). Maps based on ten years of meteorological data Each map below shows the likelihood that at a specific location the hourly ground concentration of SO2 will exceed a specific threshold. The threshold values are shown in bold blue /pollution-and-radiation/volcanic-gas/hazard-zoning

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