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• 51. Registration

  to give an oral or poster presentation, whether you intend to participate in the excursion to Langjökull on Friday afternoon, and whether you arrive on June 19 or 20. A block booking of rooms has been made at the Reykholt hotel. Potential participants are encouraged to register early due to limited number of hotel rooms. The deadline for registration was: April 15 – abstract, registration /lidar/lidar-2013/registration/

• 52. Gyrite_Brandt_(Local_Government_Denmark,_DK)

  and this was done by stakeholder involvement with different levels of involvement. The climate adaptation plan has been presented to the general public and has been used as a basis for integrating climate adaptation measures in the Municipal plan. Lolland is now an pilot study area for two Interreg projects SUSCOD and BLAST, both dealing with the coastal zone and climate adaptation. /media/loftslag/Gyrite_Brandt_(Local_Government_Denmark,_DK).pdf

• 53. Monitoring Öræfajökull – update 22. Dec. 2017

  the volcano, as assessed by the temporal changes on the ice-surface are not suggesting an increase. There are no clear indications that water is accumulating beneath the ice in the cauldron and, given the trend of the activity until now, it is unlikely to expect a flood in the next months. However, it is very important to keep following this process with regular measurements of the caldera /about-imo/news/monitoring-oraefajokull-update-22-dec-2017

• 54. A new low pressure record for July in Iceland

  21:30 to 22:30, 972.4 hPa. The pressure in Iceland has only on three occasions dropped down to 975 hPa or lower in the entire record extending back to the 1820s. These cases were 974.1 hPa in Stykkishólmur on 18 July 1901, 974.3 hPa in Stykkishólmur on 19 July 1923 and 975.0 hPa in Reykjavík 11 July 1912. It should be kept in mind that although the pressure was recorded at a few stations all /about-imo/news/nr/2504

• 55. Bardarbunga_Daily_status_report_250814

  Bárðarbunga update 25082014 2014-08-25 13:58 UTC Bárðarbunga update Compiled by Hildur María Friðriksdóttir, Benedikt G. Ófeigsson, Melissa Anne Pfeffer, Sara Barsotti, Kristjana Eyþórsdóttir Based on Seismic, GPS, Hydrology Eruption plume Height (a.s.l.) No eruption and no eruption cloud. Heading No eruption and no eruption cloud. Colour No eruption and no eruption cloud. Tephra fallout /media/jar/Bardarbunga_Daily_status_report_250814.pdf

• 56. Bardarbunga_Daily_status_report_260814

  a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga caldera is possible but presently considered to be less likely. /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 57. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 58. norsem_voss

  monthly bulletin was that of April 2015. Apart from the destructive earthquake in Italy and the nuclear explosion in the DPRK, the most significant seismic events recorded by the seismic service at GEUS in the recent period, are a sequence of earthquakes in the Disko Bay area in West Greenland. Since the beginning of the sequence on April 5th 2016, 95 earthquakes have been /media/norsem/norsem_voss.pdf

• 59. Group2-PresentationWithPictures[1]

  Scenarios for Horsens Fjord Al Azhar, Bjarke, Maria and Kerstin 26.08.2011 Scenarios for Horsens Fjord • Horsens Fjord • Policy agency and stakeholders • Several goals, focus on water quality • Backcasting to develop scenarios • Uncertainties Exploring Backcasting Collective Individual Society 3 Scenario process: socio economic Society 1 Society 2 Scenario process: climate /media/loftslag/Group2-PresentationWithPictures[1].pdf

• 60. FAQ

  ) monitors the natural hazards in Iceland closely 24/7 through real-time measurements of earthquakes, GPS and other data. In case of a sudden change in the activity, the IMO specialists alarm the Civil Protection authorities immediately which act if considered necessary in order to respond to a possible emergency. Due to the recent seismic activity on the Reykjanes Peninsula, the IMO has now /volcanoes/fagradalsfjall-eruption/faq/