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• 21. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 22. Adaptive management in relation to climate change

  to postdocs. If free places are available the course is also open to other professionals working in the subject area. Attending the course is free of charge. NONAM will provide accommodation for PhD students near the university free of charge. Participants are requested to cover travel expenses and daily allowances from their own funding. Other participants are requested to make their own /nonam/phd-summerschool/

• 23. TF-FMS_20141204_skyrsla

  on the northern site of the lava flow, minor outbreaks were observed in the southwest close to the vents and into a lava-free part in the middle of the flow, see photo on the next page. Eruption site seen from NNW, rather calm bubbling activity. Photo: Martin Hensch EBE-035-1 Eftirlitsflug /media/jar/TF-FMS_20141204_skyrsla.pdf

• 24. ESC-IASPEI-statement-LAquila-2012-1

  the free expression of scientific opinions to casualties resulting from the collapse of poorly built or maintained buildings during earthquakes, with issues and ramifications relevant to the whole seismological community: - IASPEI adheres to the statement on Freedom to Conduct Science and Responsibilities of Scientists2 of the International Union of Geophysics and Geodesy and to the principles /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 25. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 26. Glacier mapping – IPY

  km², since some ice-free areas outside the ice caps are included, and also some areas have been measured twice for research and quality assurance purposes. Comparable digital elevation models of glaciers in Iceland have hitherto not been available. The new models will serve as a baseline for comparison with all other measurement, past and future. With repeated measurements it is possible /about-imo/arctic/glacier-mapping-ipy/

• 27. Nordic Seismology Seminar in Iceland

  Thursday evening. Those who are interested in attending, are encouraged to apply for participation.The deadline for registration is 31 August. The abstract submission deadline is 15 September. The venue is Grand Hotel Reykjavík. Rooms have been reserved and can be booked through the registration process, although participants are of course free to book other accommodation.Wide range /about-imo/news/nordic-seismology-seminar-in-iceland

• 28. Glacier mapping – IPY

  km², since some ice-free areas outside the ice caps are included, and also some areas have been measured twice for research and quality assurance purposes. Comparable digital elevation models of glaciers in Iceland have hitherto not been available. The new models will serve as a baseline for comparison with all other measurement, past and future. With repeated measurements it is possible /about-imo/arctic/glacier-mapping-IPY/

• 29. Registration

  In the registration mail please send your name and e-mail, name of the institution where you work or study, and dates of arrival and departure. Participation, including 2 lunches and a dinner, is free of charge. Participants, other than speakers, have to cover travel and hotel costs themselves. Approaching Reykjavík Recreation park Heiðmörk and Reykjavík in background. Photo: Guðrún Pálsdóttir /nonam/workshop/registration/

• 30. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf