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Results:

• 11. 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

• 12. 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

• 13. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 38/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 14. Perrels-CBA

  operational cost, etc.) and the annual revenues • consider an appropriate discount rate and assess NPV (net present value), IRR (internal rate of return), and net cash flows • rank alternatives by score level • SCBA: social CBA – total benefits -/- total costs for society, in this case benefits and costs often don’t accrue (entirely) to the same organisation due to the public nature of a project /media/loftslag/Perrels-CBA.pdf

• 15. Sea ice in March 2011

  was closest to land in the following locations: 56 nm from Látrabjarg, 38 nm from Barði, 38 nm from Kögur and 50 nm from Hornbjarg. No large floes or icebergs were seen at the margin of the ice, but some scattered ice was seen off the ice edge. An observation from ship off Víkuráll was received 20th March, describing a strip of ice and large dispersed floes, implying the need of caution for passing ships /sea-ice/monthly/2011/nr/2374

• 16. 47th Nordic Seismology Seminar

  Venue 47th Nordic Seismology Seminar Venue The meeting will take place at Grand Hotel Reykjavík, Sigtún 38, 105 /norsem/norsem2016/venue/

• 17. VI_2022_006_extreme

  Þingvallavatn 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 12 15 18 19 21 23 6 hours 26 31 35 38 41 44 12 hours 48 56 62 67 73 77 24 hours 78 90 99 107 117 124 48 hours 113 128 138 148 159 168 26 Figure 12 – 1M5 map for catchment Hálslón based on the complete ICRA dataset. Figure 13 – 1M5 map for catchment Þingvallavatn based on the complete ICRA dataset. 27 5.2 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 18. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ). NeWater is based on the hypothesis that IWRM cannot be realised unless current management regimes undergo a transition towards more 0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvman.2007.05.009 Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50. E-mail address: hjh@geus.dk (H.J. Henriksen). (Downing et al., 2005). Vulnerability /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 19. Bárðarbunga 2014 - August events

  August 2014 07:10 - from geoscientist on duty Seismic activity has decreased as a result of the pressure release, however a significant amount of earthquakes is still detected in the magma dike, between the eruption site and south to about 5 km into Dyngjujökull. Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and 3.5 at 06:38 in the dike. These earthquake /earthquakes-and-volcanism/articles/nr/3000

• 20. Bardarbunga-2014_August-events

  the eruption site and south to about 5 km into Dyngjujökull. Strongest events were 3.8 in the caldera of Bárðarbunga at 04:37, as well as 2.9 at 05:39 and 3.5 at 06:38 in the dike. These earthquake are very closely monitored, but no significant change volcanic activity following these has been observed so far. Web camera from Míla shows the area. Míla's background photo has nothing to do /media/jar/Bardarbunga-2014_August-events.pdf