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• 41. VI_2020_004

  .................................................................................................................. 38 5 Results ................................................................................................................................ 39 5.1 How to read a probabilistic hazard map .................................................................... 39 5.2 Hekla /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 42. Cradden_Lucy_CES_2010

  June 2010 1 CES 2010 Climate change and UK electricity network capacity Lucy Cradden, Gareth Harrison University of Edinburgh June 2010 2 Contents • Why is electricity network capacity important – Particularly for increased renewable energy? • How does climate influence capacity? • What are the projections for UK climate change? • What effect could this have on network capacity? • How could /media/ces/Cradden_Lucy_CES_2010.pdf

• 43. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  at Springerlink.com Abstract We propose a generic framework to characterize climate change adaptation uncertainty according to three dimensions: level, source and nature. Our framework is different, and in this respect more comprehensive, than the present UN Intergovernmental Panel on Climate Change (IPCC) approach and could be used to address concerns that the IPCC approach is oversimplified. We have studied /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 44. Instructions for weather radar pages

  it encounters, i.e. mountains. This has to be considered when dealing with the Snæfellsnes peninsula and the mountain range around Reykjavík because there the reflection off the mountains is very strong. The colour scale at the bottom left corner of the image shows the strength of the reflection. The higher the number the higher the precipitation. Blue signifies low precipitation and red high /weather/articles/nr/1221

• 45. Factsheet_Bardarbunga_20141216

  of the seismic activity in Bardarbunga show a steadily decline in the seismic activity and in the number of large earthquakes.  On Saturday and Sunday, 13. and 14. December, a minor increased seismic activity was detected in the dyke and around the eruption site in Holuhraun. Between 15 and 20 earthquakes were detected each day, all smaller then magnitude M2,0. Since then about 10 earthquakes a day /media/jar/Factsheet_Bardarbunga_20141216.pdf

• 46. Factsheet_Bardarbunga_20150106

  Data collected in flight over the lava field on 30th of December show that the volume of the lava field in Holuhraun is about 1,15 cubic kilometre.  Seismic activity in Bardarbunga continues to be strong, but it has though somewhat decreased. Total number of earthquakes in Bardarbunga from the last meeting of the board, on the 30th of December, is just over 250. About 20 earthquakes were /media/jar/Factsheet_Bardarbunga_20150106.pdf

• 47. Factsheet_Bardarbunga_20150109

  appears to be similar to preceding weeks.  Seismic activity in Bardarbunga continues to be strong, but it has though somewhat decreased. Total number of earthquakes in Bardarbunga from the last meeting of the board, on the 6 of January, is just over 100. Just over 10 earthquakes were between M4,0-5,0. The strongest one was M5,1 yesterday, 8. December, at 18:47. Few earthquakes were detected /media/jar/Factsheet_Bardarbunga_20150109.pdf

• 48. Factsheet_Bardarbunga_20150120

  deflation towards Bardarbunga. • A number of monitoring equipment on and around Vatnajokull glacier are not transmitting data. A repair mission is heading towards the glacier today but weather conditions on this time of the year are very rough. • High values of sulphuric dioxide are still being recorded. Around 1800 µg/m3 SO2 were recorded last Friday in Hofn in Hornarfjordur and around 1750 /media/jar/Factsheet_Bardarbunga_20150120.pdf

• 49. Factsheet_Bardarbunga_20141112

  M4,0 and M5,0 were detected over the period. From noon on Monday the total number of earthquakes was around 130.  Very few smaller earthquakes were detected in the dyke and at the eruption site in Holuhraun.  An earthquake swarm was detected in Tungnafellsjokll glacier yesterday. The biggest earthquake was at 10:07 of magnitude M2,8.  The subsidence of the Bardarbunga caldera continues /media/jar/Factsheet_Bardarbunga_20141112.pdf

• 50. Information and help

  the danger level is classified in 5 categories according to European standards (European Avalanche Warning Services, EAWS). The forecast is made for large areas and includes both natural and human triggered avalanches. Two things are important regarding the bulletins: It is not necessarily representative for urban areas. It does not replace the assessment of individuals of conditions when travelling /avalanches/forecast/help