about 42 meters.
Energy of the geothermal areas in Bardarbunga is now few hundred megawatts and the melting of water is
estimated around 2 cubic meters per. second. The water goes into Skjálfandafljót og Jökulsá á Fjöllum. The flow is
too small to effect the total water flow of the rivers.
Around 20 smaller earthquakes are detected in the dyke and at the eruption site in Holuhraun, all
/media/jar/Factsheet_Bardarbunga_20141031.pdf
and on the road into the area making observation of the eruption more difficult for
the scientists in the field.
Seismic activity in Bardarbunga continues to be strong. Since Monday, the 3. of November, 200 earthquakes have
been detected in the caldera. The largest measured earthquake was on Tuesday, November 4. at 20:45 of M4,8. A
total of 15 earthquakes were of sizes between M 4 and 5; 15 of sizes
/media/jar/Factsheet_Bardarbunga_20141105.pdf
was analysed by Institute of Earth Sciences and is very fine grained:
24% of the sample is under 10 μm (as aerosol)
33% of the sample is in the range of 10-50 μm
20% of the sample is in the range of 50-146 μm
23% of the sample is in the range of 146-294 μm
How high is the ash plume?
The greatest height that the plume has reached is 33,000 ft (about 11 km) on the first eruption day. Early morning
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of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.).
Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1.
Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I
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list to fill
up the empty places. EUMETSAT is sending 3-5 participants representing the Baltic
countries or other member states. The number of students at the course is 20-25.
Finances
The host country is responsible for the finances and reports to EUMETSAT and its own
Economy department.
There is no course fee.
The host country covers the cost for its own participants and teachers. The host
/media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf
Clausen, N.-E., Pryor, S. C., Guo Larsén, X., Hyvönen, R., Venäläinen, A., Suvilampi, E., Kjellström, E., Barthelmie, R. (2009). Are we facing increasing extreme winds in the future? EWEC 2009 Marseille session DT2A, 19 March 2009.
Engen-Skaugen,T & Førland, E.J. (2010). Future change in return values and extreme precipitation at selected catchments in Norway, met.no Report 20/2010 (draft).
Engen
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