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• 41. Supporting structures stopped most of an avalanche

  ). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover /about-imo/news/nr/2476/

• 42. Supporting structures stopped most of an avalanche

  red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures /avalanches/articles/nr/2475/

• 43. Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO

  Sólheimajökull. Samples of the water have been collected for analysis. Conditions at eruption site: The eruption sight was not visible today. From the flight of the Icelandic Coast Guard (ICG) 04.05.2010: The crater continues build up in the northern most ice cauldron. Lava flows to the north and spreads at 500 m a.s.l. The lava tongue is about 200 m wide and lava channels that join /media/jar/Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO.pdf

• 44. Further information regarding gas pollution

  rather than towards you.In calm/light wind (<5 m/s) gas can accumulate in the valleys, then circulation is controlled by the landscape and gas can exceed danger levels far up the slopes, all around the eruption site. In such cases, spectators need to move up to higher ground levels such as mountains and ridges and not stay on the slopes just above the eruption. Choose a walking route according /volcanoes/fagradalsfjall-eruption/volcanic-gases/

• 45. Rolf_Johnsen_(Region_Midt,_Dk)

  standards. It will also change the available groundwater resource and stream flow patterns between summer and winter. Rising sea levels will also affect the development of recreational areas and water abstraction in coastal zones because of flooding and seawater intrusion into fresh aquifers. Climate change scenarios pose great challenges to adaptive local and transboundary spatial planning /media/loftslag/Rolf_Johnsen_(Region_Midt,_Dk).pdf

• 46. Supporting structures stopped most of an avalanche

  of the structures is approximately at the elevation of the top row it is not clear whether the snow cover above the structure would have been released as an avalanche in the absence of the structures. In a few locations one could see that the avalanche slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may be assumed /about-imo/news/nr/2476

• 47. Supporting structures stopped most of an avalanche

  to the west of the structures is approximately at the elevation of the top row it is not clear whether the snow cover above the structure would have been released as an avalanche in the absence of the structures. In a few locations one could see that the avalanche slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may /avalanches/articles/nr/2475

• 48. Gode_Jenny_CES_2010

  square4 The task square4 Results and reflections square4 Summary Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 Production potentials Climate change Energy demand Physical impact, damage Background: Climate change will affect the whole energy system Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 The task square4 Stakeholder dialogue; How can the energy sector use /media/ces/Gode_Jenny_CES_2010.pdf

• 49. 2011_005

  transfer and preparation. 3. Assessment of IP-based communication options for dial-up connections. 4. Review of station locations and possibilities for network optimization. 5. Appraisal of data processing, including existing drawbacks, alternative software, future needs for monitoring purposes, data archival, and sharing of CGPS data. 8 1.3 Modifications to original aims As work progressed /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 50. Bad weather is expected

  in the afternoon. Becoming moderate southwesterly winds tomorrow evening, with showers of rain or sleet.The weather moves to the northwest over the country and becoming strong winds also in the north and east part in the afternoon. The most severe conditions there will be there in the evening, southeasterly 20-28 m/s and gusts up to 40 m/s in the mountains. Winds moderating after midnight.Heavy rain /about-imo/news/bad-weather-is-expected-1