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  • 11. VI_2016_006_rs

    landslides that caused accidents or damage to property, were documented in the early part of the 20th century. In the last decades, most landslides that have occurred near the settlement have been recorded. The location of at least 100 landslides within the settlement or in close proximity to it are known and it may be estimated that the total number of landslides in area since 1882 is at least 3–4 times /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
  • 12. IPPC-2007-ar4_syr

    about 28% and losses from the polar ice sheets contributing the remainder. From 1993 to 2003 the sum of these climate contributions is consistent within uncertainties with the total sea level rise that is directly observed. {WGI 4.6, 4.8, 5.5, SPM, Table SPM.1} Observed decreases in snow and ice extent are also consistent with warming (Figure 1.1). Satellite data since 1978 show that an- nual average /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 13. Factsheet_Bardarbunga_20141031

    continues to be strong. 200 earthquakes have been detected in the caldera over the last 48 hours. Just over ten earthquakes were bigger then magnitude M4,0. The largest one was M5,3 tonight at 01:30.  The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as it has done over the last few weeks. The total depression in the caldera is now /media/jar/Factsheet_Bardarbunga_20141031.pdf
  • 14. Factsheet_Bardarbunga_20141112

    to grow to the south. Yesterday a helicopter from the Icelandic Cost Guard used to examine conditions by the southern edge of the lava field, were lave is flowing on a 3-5 km wide area.  Seismic activity in Bardarbunga continues to be strong. The biggest earthquake that was detected over the last two days was on Monday, 10. November at 22:39 of magnitude M5,2. In total 15 earthquakes between /media/jar/Factsheet_Bardarbunga_20141112.pdf
  • 15. Factsheet_Bardarbunga_20141114

    Convection of sulphuric dioxide from the crater appears to be constant.  Seismic activity in Bardarbunga continues to be strong but number of earthquakes stronger then M5,0 seem to be decreasing. The biggest earthquakes that were detected over the last two days were yesterday, 13. November at 20:46 of magnitude M4,9 and at 23:08 of magnitude M4,8. In total 17 earthquakes bigger then M4,0 were /media/jar/Factsheet_Bardarbunga_20141114.pdf
  • 16. Factsheet_Bardarbunga_20141117-1

    The Lava field is now about 72 square kilometres. • Seismic activity in Bardarbunga continues to be strong. The two biggest earthquakes that were detected since noon on Friday were both of magnitude M5,4. On Friday, 14. November at 11:25 and on Sunday, 16. November, at 01:37. In total 16 earthquakes bigger then M4,0 were detected over the period and 25 earthquakes between M3,0-3,9. In total 160 /media/jar/Factsheet_Bardarbunga_20141117-1.pdf
  • 17. Factsheet_Bardarbunga_20141119

    in the crater to east southeast.  Seismic activity in Bardarbunga continues to be strong. The two biggest earthquakes that were detected since noon on Monday were both of magnitude M4,6. On Tuesday, 18. November at 18:21 and on tonight, 19. November, at 00:29. In total 16 earthquakes bigger then M4,0 were detected over the period and 51 earthquakes between M3,0- 3,9. In total 200 earthquakes were /media/jar/Factsheet_Bardarbunga_20141119.pdf
  • 18. The weather in Iceland 2010

    except in January and September. The annual total was only 74% of the mean. In Stykkishólmur the precipitation has been measured almost continuously since 1856 (a few months in 1919 are missing). 2010 was the fifth driest of the series; it was driest 1881, 1915, 1916 and 1998. The annual total was only 65% of the annual average. In the North and East the total precipitation in 2010 was slightly /about-imo/news/2011/nr/2112
  • 19. The weather in Iceland 2010

    except in January and September. The annual total was only 74% of the mean. In Stykkishólmur the precipitation has been measured almost continuously since 1856 (a few months in 1919 are missing). 2010 was the fifth driest of the series; it was driest 1881, 1915, 1916 and 1998. The annual total was only 65% of the annual average. In the North and East the total precipitation in 2010 was slightly /about-imo/news/nr/2112
  • 20. ved-eng-2010

    from 1907 to 1920. During that time the years 1915, 1916 and 1917 were very dry in the area. The precipitation in Reykjavík was below the average in all months except in January and September. The annual total was only 74% of the mean. In Stykkishólmur the precipitation has been measured almost continuously since 1856 (a few months in 1919 are missing). 2010 was the fifth driest of the series /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

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