Grímsvötn volcano
Status Report: 17:00 GMT, 4 November 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: Thorunn Skaftadottir, Eyjólfur Magnússon, Snorri Zophoniasson,
Steinunn S. Jakobsdottir, Gunnar B. Gudmundsson and Matthew J.
Roberts.
Based on: IMO seismic monitoring; IMO hydrological data; IES-IMO GPS
monitoring
Meltwater
/media/vatnafar/flod/Grimsvotn_status_2010-11-04_IES_IMO.pdf
Eruption in Eyjafjallajökull
Status Report: 15:00 GMT, 1 June 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University
of Iceland
Compiled by: Gunnar B. Guðmundsson, Helga Ívarsdóttir, Sibylle von Löwis and Sigrún
Hreinsdóttir
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data;
web cameras, ATDnet – UK Met. Offices lightning detection
/media/jar/Eyjafjallajokull_status_2010-06-01_IES_IMO.pdf
Grímsvötn volcano
Status Report: 16:00 GMT, 26 May 2011
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: Sigurlaug Gunnlaugsdóttir, Gunnar B. Guðmundsson and Björn
Oddsson, with input from Gunnar Sigurðsson, Þórður Arason, Matthew
J. Roberts, Sigrún Hreinsdóttir and Sibylle von Löwis.
Based on: IMO seismic monitoring; IES-IMO GPS
/media/jar/Grimsvotn_status_2011-05-26_IES_IMO.pdf
operational and economic aspects
13:30 Operational aspects and economic implications of the volcanic ash issue Asgeir Pálsson, Isavia.
14:00 Impact of ash crisis on Icelandair operations, Hilmar B. Baldursson, Matthías Sveinbjörnsson
Possible near field models for Iceland
14:30 High resolution models and use of NAME at IMO Guðrún Nína Petersen, Halldór Björnsson,
Sigurður Jónsson and Sigurður
/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
between
/norsem/norsem2016/program/poster
than 30,000 earthquakes at 5–7 km depth, advancing in short bursts at 0.3–4.7 km/h. Following each
surge forward, the seismicity behind the dyke tip dropped, implying that the subsequent dyke opening
was mostly aseismic. More detailed analyses of the seismic data recorded by a dense network around
the Vatnajökull icecap have revealed small magnitude, long-period (LP or B-type) events which
/media/norsem/norsem_bryndis.pdf
The recent Bothnian Bay M4.1 earthquake: where, how and why?
B. Lund1, M. Uski2, H. Shomali1, D. Buhcheva1, S. Amini1, J. Kortström2
1Dep. of Earth Sciences, Uppsala University, Sweden
2Institute of Seismology, Dep. of Geosciences and Geography, University of Helsinki, Finland
On 19 March 2016 a magnitude 4.1 earthquake occurred in the Bothnian Bay, between northern
Sweden
/media/norsem/norsem_lund.pdf
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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
). Distribution of snow accumulation on the Svartisen ice cap, Norway, assessed by a model of orographic precipitation. Hydrological Processes, 22(19), 3998-400.
Other international
Crochet, P., Jóhannesson, T., Sigurðsson, O., Björnsson, H. & Pálsson, F. (2008). Modeling precipitation over complex terrain in Iceland. In: Sveinsson, Ó. G. B., S. M. Garðarsson and S. Gunnlaugsdóttir (eds.), Northern
/ces/publications/nr/1940