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• 21. Reykholt-abstracts

  of 2.7 km2 (20%) and a volume loss of 0.4 km³ (30%). A surface lowering of 180 m is observed near the snout decreasing to negligible amounts above 1700 m elevation. This minimal surface lowering at high altitudes is supported by a comparison of the elevation of trigonometrical points on the plateau of Öræfajökull from the Danish General Staff map of 1904 and a recent lidar-based digital elevation /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 22. askja_minnisblad_ens

  Minnisblað ___________________________________________________ 7 Figure 8. Right: An areal photo of the rockslide area in Suðurbotnar. There is evidence of older movement which is probably an old rockslide. Left: The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 23. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  ° latitude-longitude grid. However, for the present analysis we aggregated the data to a somewhat coarser 0.5° × 0.5° grid. This was done for reducing the computing burden; the loss of information associated with this aggregation is most likely minimal. Table 2.2 The RCM simulations used in this report. Institution refers to the institution that conducted the RCM simulation. The model /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 24. Update on activity in Eyjafjallajökull 2010

  Photo: Steinunn Jakobsdóttir. On ashfall - 23 May 2010 11:45 The eruption activity is minimal and therefore no significant ashfall is expected. The volcano is still being monitored and an ashfall forecast will be issued if neccessary. Assessment - 22 May 2010 16:30 According to reconnaissance flight at 14:00, the plume is estimated at 4km/14,000ft height (a.s.l.). The plume is lightgrey /earthquakes-and-volcanism/articles/nr/1884

• 25. Kok_et_al._TFSC_published_2011

  exploratory scenarios (narrative storylines) were developed, in first instance based on a set of existing European scenarios. Results matched expectations; the process produced stories that are complex, integrated, and rich in detail. During the backcasting exercise, four timelines were constructed, each of which took one exploratory scenario as context. The backcasting process established a strong link /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 26. The weather in Iceland 2012

  but the damage was minimal, without doubt because of the large mitigating effort which has been ongoing for the last 17 years. Temperature The year was warm, especially in the western part of the country. In Stykkishólmur in the west it was the seventh warmest year since the official start of observations in 1845. There and in Reykjavik it was the 17th in an unbroken sequence of above normal [1961 /weather/articles/nr/2614

• 27. ved-eng-2012

  days. Many residential and industrial buildings had to be evacuated for a few days due to a threat of avalanches, which hit several structures but the damage was minimal, without doubt because of the large mitigating effort which has been ongoing for the last 17 years. Temperature The year was warm, especially in the western part of the country. In Stykkishólmur in the west it was the seventh /media/vedurstofan/utgafa/skylduskil/ved-eng-2012.pdf

• 28. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  : The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit, the edge seems to have advanced (purple area). Background: Loftmyndir ehf. Analyses: Ásta Rut Hjartardóttir and Þorsteinn Sæmundsson. Fig. 9 Figure 9. Geological map showing the outline of the rockslide, as well as eruptive fissures /avalanches/articles/nr/2929

• 29. Information and help

  The classification is based on the destructive potential of the avalanche, and it has been slightly modified for Icelandic conditions. The table also gives a typical mass in tons. Size Destructive potential Mass 1 Minimal danger of burying (danger of falling). 10 tonn 2 Could bury, injure or kill a person. 100 tonn 3 Could bury and destroy a car, damage /avalanches/forecast/help

• 30. Paper-Olafur-Rognvaldsson_92

  are enclosed in black boxes. behaves differently in N- and S-Iceland for stations in flat land (minimal effect of non-resolved orography). For stations on flat land in the South, the simula- tions and observations are in an overall reasonable agreement (see stations in blue boxes in Fig. 1). The model does however underestimate precipitation in flows from the SE (not shown). The model overestimates /media/ces/Paper-Olafur-Rognvaldsson_92.pdf