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• 61. Earthquake swarm on the Reykjanes ridge

  :25 last night and it was well felt on the peninsula and in the capital area, as well as on a ship around 10 km away from the epicenter. A few more events of magnitudes between M4 and M5 have been detected since the onset of the swarm, and are still under manual revision. As the swarm is taking place offshore and outside the IMO monitoring network, further data and information had to be requested /about-imo/news/nr/3160

• 62. The earthquake swarm on Reykjanes ridge

  midnight and activity is since occurring in pulses with two to three hours in between. The strongest earthquakes detected since the onset of the swarm were M5.0 at 02:25 and M4.9 at 04:59 on the morning of 1 July. Similar swarms have been recorded in previous years and have generally lasted up to a couple of days without resulting in an observable eruption. Indeed, the area is known for frequent /about-imo/news/nr/3163

• 63. Warning due to intense rainfall

  winds (20 - 25 m/s) yesterday that affected southern and western regions. Prolonged rainfall is continuing to affect the west, south, and south-east of the country. The storm will be followed closely by another low tonight, Wednesday evening, 9 September, which will bring intense rainfall to south-east Iceland and, for a time, the Snæfellsnes peninsula. Rising stream and river levels are expected /about-imo/news/nr/3187

• 64. Earthquake sequence offshore North Iceland

  and slightly southwest of the seismic sequence observed last September. The strongest earthquakes occurred on early Sunday morning, 21 October, at 00:10 (M4.8) and 01:25 (M5.6). The stronger event came first up as M5.2 but has been revised to M5.6 by including seismic data from mainland Europe, Greenland and Northern America. It was widely felt in North Iceland, from Ísafjörður to Seyðisfjörður /about-imo/news/nr/2555

• 65. 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

• 66. Eyjafjallajokull_status_2010-05-25_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 17:00 GMT, 25 May 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: Hjörleifur Sveinbjörnsson, Þorsteinn Jónsson, Björn Sævar Einarsson and Sigrún Hreinsdóttir Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data; web cameras, ATDnet – UK Met. Offices lightning /media/jar/Eyjafjallajokull_status_2010-05-25_IES_IMO.pdf

• 67. Eyjafjallajokull_status__2010-04-25_IES_IMO

  Eruption in Eyjafjallajökull – status report 25 April 2010 at 1800 from Icelandic Meteorological Office and Institute of Earth Sciences, UoI Compiled by: MTG / SSJ Based on: IMO seismic monitoring, IES/IMO GPS monitoring, IMO river gauges, information from local police and IES geologists inspection of tephra Eruption plume: Height( a.s.l): Unknown, not seen above cloud cover /media/jar/Eyjafjallajokull_status__2010-04-25_IES_IMO.pdf

• 68. Registration

  for Sunrise in the Barents Sea 25 February 2007. Photo: Skúli Eggertsson. Core Partners Finnish /nonam/phd-summerschool/registration/

• 69. Call for abstracts

  to submit abstracts for poster presentations under the three workshop topics. Abstracts will be evaluated by a scientific committee. Abstracts will be published in the abstract booklet given to all conference visitors. Abstract submission guidelines Submission only by e-mail to hanna.virta@fmi.fi Submission deadline for initial abstracts: 25 June 2010 Notification for acceptance (by e-mail): 5 /nonam/workshop/abstracts/

• 70. CES_D2.4_task2_CMIP3_winds

  ° latitude-longitude grid. Verification One grid point (60°N, 25°E) was selected for comparing the surface geostrophic wind speeds in the 10 GCMs with the corresponding observed geostrophic winds, which were derived from the ERA-40 reanalyses. In general, the monthly average Vg in the model simulations was found to be nearly equal to the corresponding observed mean (Fig. 1). However, during /media/ces/CES_D2.4_task2_CMIP3_winds.pdf