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• 41. VI_2019_009

  26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 250 500 750 250 500 750 Number of records Figure 15. Automatic station as a function of manual station. a71 a71a71a71a71a71 a71a71 a71a71a71 a71a71 a71 a71 a71a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71a71a71 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 42. VI_2015_007

  of Iceland, Science Institute, University of Iceland, and National Energy Authority. 2004), a soil map from the Agricultural University of Iceland and a vegetation map from the Icelandic Institute of Natural history were also used in this study. 8 Table 1. Main characteristics of river basins used in this study. Catchment Name Area Mean Mean annual Available period / (km2) elevation precipitation /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 43. Protective measures

  to the "Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Rep. 99013)" (IMO Memo TóJ-2003-05, author T. Jóhannesson) (pdf 0.03 Mb) Remarks on the design of avalanche braking mounds based on experiments in 3, 6, 9 and 34 m long chutes (IMO Int. Rep. 03024, 2003, authors T. Jóhannesson and Kr. M. Hákonardóttir) (pdf 0.8 Mb) Field observations and laboratory /avalanches/imo/protective/

• 44. Activity in the Bárðarbunga system since the end of the eruption

  year's expedition. The depth and width of the cauldrons has not been measured for quite some time, such measurements can only be carried out with airborne surveillance. Therefore no statement can be made on changes in geothermal activity from last year. A new seismographic station was installed at approximately 1600 meters elevation northwest of the Bárðarbunga caldera on June 5th. The station /about-imo/news/activity-in-the-bardarbunga-system-since-the-end-of-the-eruption

• 45. New seismic stations installed around Öræfajökull

  to be very beneficial to locate earthquakes in this volcanic area.When looking at long-term changes in the seismicity, activity has been increasing in Öræfajökull since 2016. In June and since early September this year, the activity has increased still further. The new stations are therefore an important addition to the pre-existing monitoring network for improving the sensitivity /about-imo/news/new-seismic-stations-installed-around-oraefajokull

• 46. Bárðarbunga GPS displacements

  by the propagation of the dyke had become negligible, and from then on the displacement signals from stations around Bárðarbunga can be directly linked to the subsidence of the caldera. Monitoring ceased 19 April 2015. Enlarge. The dates are explained below. Terms, see bottom of page. Dates (yyyymmdd-yyyymmdd) above the cm/year legend. As an example, 20141213-20150113 represents displacement velocities /earthquakes-and-volcanism/gps-measurements/bardarbunga/

• 47. A year since the Eyjafjallajökull eruption began

  the eruption, it was necessary to hold frequent meetings with aviation authorities, flight companies, communities in the vicinity of the volcano and civil protection authorities. IMO was guided by London VAAC, one of the volcanic ash advisory centres. In September 2010, after the eruption, an Atlantic Conference on Eyjafjallajökull and Aviation was held. The Keilir Aviation Academy organized /about-imo/news/nr/2164

• 48. Workshop on Earthquakes in North Iceland

  of Akureyri Institute of Earth Sciences, University of Iceland KAUST, King Abdullah University of Science and Technology Húsavík Academic Center Icelandic Meteorological Office Earthquake Engineering Research Centre, University of Iceland Civil Protection Department, National Commisioner of the Icelandic Police Iceland Catastrophe Insurance Husavik Academic centre Ministry of the Interior /about-imo/news/nr/2701

• 49. A year since the Eyjafjallajökull eruption began

  the eruption, it was necessary to hold frequent meetings with aviation authorities, flight companies, communities in the vicinity of the volcano and civil protection authorities. IMO was guided by London VAAC, one of the volcanic ash advisory centres. In September 2010, after the eruption, an Atlantic Conference on Eyjafjallajökull and Aviation was held. The Keilir Aviation Academy organized /about-imo/news/2011/nr/2164

• 50. PhD Workshop 2012

  decision support models and procedures and processes applied in analyzing, planning and implementing adaptation to climate change. Virtually all sub-themes mentioned in the Conference call, as well as many others not described, can be related to the practical uptake of adaptation. Studies, that address sectoral or regional dimensions of adaptation, are of particular interest. Character /nonam/adaption/phd-workshop-2012/