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• 21. Bárðarbunga 2014 - August events

  August 2014 07:10 - from geoscientist on duty Seismic activity has decreased as a result of the pressure release, however a significant amount of earthquakes is still detected in the magma dike, between the eruption site and south to about 5 km into Dyngjujökull. Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and 3.5 at 06:38 in the dike. These earthquake /earthquakes-and-volcanism/articles/nr/3000/

• 22. Hazard zoning

  : Estimation of avalanche risk (IMO Rep. VÍ-R99001-ÚR01, authors K. Jónasson S. Þ. Sigurðsson and Th. Arnalds) (pdf 0.5 Mb) Avalanche hazard zoning in Iceland based on individual risk (Annals of Glaciology, 38, 285−290, 2004, authors Th. Arnalds, K. Jónasson and S. Þ. Sigurðsson) (pdf 0.4 Mb) A map on a selected front page shows recent observations of avalanches. For user access /avalanches/imo/hazard/

• 23. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 24. hafisskyrsla-23-mars-2011

  2. 66°03N 026°18V 3. 66°10N 026°01V 4. 66°24N 025°18V 5. 66°58N 023°21V 6. 67°03N 023°24V 7. 67°33N 022°26V Var ísröndin næst landi: 56 sml frá Látrabjargi. 38 sml frá Barða. 38 sml frá Kögri. 50 sml frá Hornbjargi. Veður: V 10-23 kt léttskýjað og gott skyggni. Viggó M. Sigurðsson Stýrimaður. /media/hafis/skyrslur_lhg/hafisskyrsla-23-mars-2011.pdf

• 25. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 26. Seismic activity still great

  than those described above, have occurred in Bárðarbunga, where the activity started. This is the same pattern as during previous days. The highest magnitude during the last 24 hours was about 3.8, measured at 23:38 last night (20th August). In addition to the news Additional material on the web, now available in English, can be found through links on the long banner at the top of our front page /about-imo/news/nr/2951

• 27. Registration

  There are 38 registered participants who will present 20 oral presentations and 10 posters. Search Search string /lidar/lidar-2013/registration/

• 28. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 29. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf

• 30. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf