15.0W
9) 67 05.0N 21 52.0W
10) 66 57.0N 22 32.0W
11) 67 00.0N 23 00.0W
12) 66 38.0N 25 00.0W
13) 66 30.0N 26 40.0W
Næst landi var ísinn á eftirfarandi stöðum:
1. 48 sjml vnv af Grímsey.
2. 46 sjml ana af Horni.
3. 34 sjml norður af Skagatá.
4. 25 sjml nnv af Sraumnesi.
Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að
sigla í gegnum
/media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
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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& 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
/ces/publications/nr/1943
Journal of Environmental Psychology, 26, 15-26. doi:10.1016/j.jenvp.2006.05.003
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.
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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
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