K. Maack, Director General Icelandic CAA
Ash measurements, experience 2010 and 2011
9:45 Eruptions in Eyjafjallajökull, Etna and Grímsvötn, airborne OPC measurements and quality
assurance Konradin Weber, UAS, Düsseldorf Germany
10:15 Observations in plumes and vicinity of airports Jonas Eliasson HÍ (UI)
Initial and boundary data acquisition and improvements in modelling
10:45
/media/vedurstofan/utgafa/hlidarefni/program17012012.pdf
on Intraplate Seismicity in Central Fennoscandia
Annakaisa
Korja, Uski, M., Lund, B., Grigull, S., Nironen, M., E., Högdahl, K. Relative earthquake location in
Southern Iceland Bergþóra S. Þorbjarnardóttir and
Ingi Þ. Bjarnason This year's update on the Burträsk
fault seismicity Darina Buhcheva
and Björn LundThe SIL-system from an operational standpointJón Söring
Communication
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finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
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& Hannah, D.M. (2010). Regional hydrological drought in north-western Europe: linking a new Regional Drought Area Index with weather types. Hydrological Processes , 24 (in press), doi: 10.1002/hyp.7644.
Fleig, A., Tallaksen, L.M., Hisdal, H., Stahl, K. & Hannah, D.M. (2009). Inter-comparison of weather and circulation type classifications for hydrological drought development. Physics
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Hare M P, Krywkow J (2005) Participatory processes for the design of water storage areas. Technical report, Seecon Deutschland GmbH, Osnabrück. Seecon TR
no. 01/2005 for the EU Interreg IIIB TRUST project. Short version available in electronic format.
Kok K (2009) The potential of Fuzzy Cognitive Maps for semi
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were carried out to obtain the flow and
sliding parameters for Hoffellsjökull that resulted in a good
simulation of the observed 20th century evolution of the
glacier geometry. The obtained values for the rate factor
and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and
C = 10× 10−15 m a−1 Pa−3, respectively.
The ice divide is kept at a fixed location in the model com-
putations presented here
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
surface.
As a simple scale of Aurora activity we use the Kp-index, which describes strength of variations in the magnetic field of the Earth. The Kp-index is from 0 to 9, where 0 describes minimum activity and 9 maximum. Most of the time the Kp-index is 0-3 and the highest numbers are very rare. The Kp-index is calculated as a weighted mean of K-indices from many magnetic observatories around
/weather/articles/nr/2549