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• 51. 2011_005

  receiver since 22-04-2011 SNAE Snæbýli ? Off-line due to hardware failure with the receiver 10 Some of these stations are difficult to get back online without site visits. Consequently they may therefore be out-of-service for extended periods. Based on an estimate of the completeness of the GPS data-set in 2010, the uptime of the network is about 70.5%. For further details, see section 6 /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 52. 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

• 53. 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/

• 54. 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

• 55. 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/

• 56. 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/

• 57. 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

• 58. James-Smith_Edward_CES_2010

  opportunity evaluation Case studies NOE Net SEAS-NVE Findings of case studies • Distribution companies generally well equipped for climate change – Cabling of all overhead lines well under way – Distribution boxes in areas with increased risk of flooding are elevated already – Salt spray further inland is becoming an increasing problem for substations and transformers Cabling in Denmark /media/ces/James-Smith_Edward_CES_2010.pdf

• 59. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 60. NONAM conference in August

  or Workshop in Reykjavík. Participation, including 2 lunches and a dinner, is free of charge. Participants, other than speakers, have to cover travel and hotel costs themselves. Participants are invited to bring a poster of their projects. Abstracts for posters are to be submitted before 1st July to hanna.virta@fmi.fi. Notification of acceptance is given in early July. Guidelines: maximum /nonam/news/nr/1932