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21. Articles

22. norsem_martin

for the time period 2001–2009, obtained from the permanent SIL network, were analysed to study stress changes associated with the main shocks. Results reveal a coseismic counter-clockwise rotation of the maximum horizontal stress of 11 ± 10° (95 per cent confidence level) in the main rupture region. From previous fault models obtained by inversion of geodetic data, we estimate a stress drop /media/norsem/norsem_martin.pdf

23. Paper-Olafur-Rognvaldsson_91

the opportunity to model river runoff and glacier mass balance both in the current climate and also in a hypothetical future climate based on the CE /VO climate change scenarios. The climate of Iceland is largely governed by the interaction of orography and extra-tropical cyclones, both of which can be described quite accurately by present day atmospheric models. As a result, dynamical downscaling /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

24. New web for mobiles

This is the most frequently accessed information on our main web and should be of use to travellers and tourists who do not have access to the internet, except via their mobiles. In July this service will be extended. Wind, temperature and precipitation forecasts will be available, as well as information on recent earthquakes and the level of some main rivers. With further improvement, IMO's mobile /about-imo/news/nr/1612

25. News

26. News

Met Office's main weather station for Iceland 1881-1920, then a manned station of the Icelandic Met Office, and now an automatic weather station. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/bigimg/3273

27. Glacier-outburst flood from Mýrdalsjökull

conduction early evening on 8th July, around the time of peak in the tremor. The water level reached the bridge around midnight, causing damage to the sensors. Contact to the instruments was lost a few hours later. Another gauging station is at Selfjall, ment for registration of flood heights as well as a part of the warning system. It is normally not in the water. Around 4 am 9th July, it began /about-imo/news/nr/2236

28. Earthquake activity offshore North Iceland continues

of the main cluster where the M5.6 event occurred on Sunday morning. Yesterday's cluster is located slightly closer to the Húsavík Flatey Fault and strongest events were around M3.9 at 05:25 and 05:32. Another M3.5 earthquake at 21:16 on 22. October and an earthquake M4.0 at 05:27 on 23. October were again located in the area of the M5.6 main shock further northwest. These earthquakes are purely /about-imo/news/nr/2558

29. 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

30. Sea ice maps from the Danish Meteorological Institute

Institute (DMI) presents ice maps. The maps are either based on satellite images or reconnaissance flights from Greenland. Various DMI ice-maps are available on their web (see dates as links below the main map). Their latest maps are also accessible through our web: Newest map (in black and white) (pdf 0,7 Mb) Newest map (in colour) (pdf 0,7 Mb) Ice chart colour code standard (WMO 2004 JCOMM /sea-ice/sea-ice-maps/dmi/

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