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• 21. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 22. vonKorff_etal-2010

  played a role in this first phase as the author tables on decision analysis show. In summary, the comparison resulted in the reconstruction of 10 steps on which there appears to be considerable agreement among the five guides. 1. DA 1: Assemble a team for decision analysis as part of the participation design. Its members should belong to the lead agency, e.g., the water board, but can also /media/loftslag/vonKorff_etal-2010.pdf

• 23. Factsheet-Bardarbunga-140901

  -area. This corresponds to a magma discharge of 300 to 500 cubic metres per second. From observations yesterday evening, the volume of erupted lava is between 16 and 25 million cubic metres. The eruption has not created any ash-fall. Gas and steam rises to a couple of hundred metres above the eruption site, extending up to 1,200 m downwind. In connection with the FUTUREVOLC project, a gas /media/jar/Factsheet-Bardarbunga-140901.pdf

• 24. Climate and Modeling Scenarios

  & Ruosteenoja, K. (2009). Comparing regional risks in producing turnip rape and oilseed rape - Impacts of climate change and breeding. Acta agriculturae Scandinavica 59B:2, 129-138. doi:10.1080/09064710802022895 (http://www.ingentaconnect.com/content/tandf/sagb/2009/00000059/00000002/art00004). Pryor, S.C., Barthelmie, R.J., Clausen, N.E., Drews, M., MacKellar, N. & Kjellström, E. (2010). Analyses /ces/publications/nr/1680

• 25. Map of the glaciers of Iceland

  at the peak of the so called Little Ice Age during the 1890s and also the outlines as they were around the year 2000. The map distinguishes surging glaciers from other outlet glaciers, and identifies all known sub-glacial volcanic calderas. Featured are the names of all named glaciers and the map includes a brochure and a list of glacier names. The Map of Glaciers can be used for both tourism /about-imo/arctic/map-of-glaciers/

• 26. Glaciologists meet in Iceland

  changes in a wider societal context were also on the agenda. Participants visited the geothermal baths of Krauma and the 500 m long man-made ice tunnel in Langjökull ice cap, pictured above. (Photo: IMO) A 2-day beginner Elmer/Ice course took place in Reykjavík prior to the Nordic Branch meeting, for researchers and students aiming to start working with Elmer/Ice. The course was sponsored /about-imo/news/nordic-glaciologists-meet-in-iceland

• 27. VONA message

  13:15:50 UTC in Meradalir (within the Fagradalsfjall system). An helicopter flight has confirmed its position to be 63 53,84N - 22 14,58W. The eruption is visible on webcameras and is taking place just north of Fagradalsfjall within the old lava field. Lava is extruded by a fissure about 300 m long. No ash is detected in the atmosphere. The aviation color code is moved back to orange /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 28. Grimsvotn_status_2010-11-02_IES_IMO

  continues to increase at seismic station ‘grf’, located near Grímsvötn. This tremor is similar in character to the tremor that accompanied the jökulhlaup in November 2004. Presently, there is no sign of volcanic tremor. Earthquakes: Two earthquakes occurred beneath Grimsvötn yesterday evening: 18:50 GMT and 20:59 GMT. Today, two earthquakes have been recorded: 06:06 GMT and 06:42 /media/vatnafar/flod/Grimsvotn_status_2010-11-02_IES_IMO.pdf

• 29. Grimsvotn_status_2010-11-04_IES_IMO

  : The jökulhlaup in the Gígja river peaked yesterday between 13:00 and 14:00 GMT at ~2,600 m3/s. At 10:30 GMT today, a discharge of 1,005 m3/s was recorded. The electrical conductivity of floodwater draining beneath the Gígja bridge remains high, with values of over 500 µS/cm measured today. Seismic tremor: Tremor levels at seismic station 'grf' are declining rapidly. There is no sign of low /media/vatnafar/flod/Grimsvotn_status_2010-11-04_IES_IMO.pdf

• 30. 47th Nordic Seismology Seminar

  on the respective day. Poster presentations (during all three coffee breaks) Tuesday 11 October Arrival and check-in. Most flights will arrive in the afternoon, so you should be at your hotel around 17:00/18:00.19:00 Kickoff party at IMO (Bústaðavegur 7, 108 Reykjavík). We will meet you at 18:30 outside Grand Hotel and walk together to IMO. Should anybody prefer to get a lift by car, please /norsem/norsem2016/program/