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• 21. 2005EO260001

  ) that a volcanic eruption seemed inevitable. Multidisciplinary Monitoring of the Eruption At 1930 UTC on 1 November, seismicity in- creased again. By 2000 UTC, earthquakes were continuously occurring and seismic tremor on nearby stations soared (Figure 3), suggesting the beginning of a volcanic eruption. On this premise, IMO sent a warning at 2010 UTC to the NCPA and OACC that a subglacial /media/jar/myndsafn/2005EO260001.pdf

• 22. aerodrome_summaries_20140603

  ) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME (UTC) <800 <1500 <3000 <8000 <200 <500 <1000 <2000 0 1 1 3 9 1 1 2 3 9 2 1 2 3 9 3 1 2 3 9 4 1 2 3 9 5 1 2 3 9 6 1 2 3 9 7 1 2 3 9 8 1 1 3 9 9 1 1 3 9 10 1 1 3 9 11 1 1 3 /media/vedur/aerodrome_summaries_20140603.pdf

• 23. VI_2009_002rs

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf

• 24. 2010_003rs

  to “bookshelf” type faulting. In June 2000, two large earthquakes of magnitudes ML6.4 and ML6.5 struck in the SISZ, three and a half days and approximately 17 km apart. Seismicity greatly increased in all Southwest Iceland and during 2000, roughly nineteen thousand microearthquakes were recorded there. The aim of this research is to relocate the earthquakes using a double- difference relative /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 25. VI_2013_008

  A A A A A Vatnajökull Mýrdalsjökull Hofsjökull Langjö k ull Drangajökull VHM-66 VHM-19 VHM-10 VHM-145 VHM-64 VHM-26 0 10050 Km A Gauging StationWatershedGlacier A m.a.s.l1 - 200200 - 400400 - 600600 - 800800 - 10001000 - 12001200 - 14001400 - 16001600 - 18001800 - 2000 Figure 1. Topography of Iceland and location of watersheds considered here. Table 1. Characteristics of the considered watersheds. Letter /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 26. Early work and an overview of measurements

  for more than 80 years in most parts of the country. Back to top Additional material and references: Trausti Jónsson og Hilmar Garðarsson 2001. Early Instrumental Meteorological Observations in Iceland. Climatic Change 48, 169-187. Ogilvie, A. E. J. og Trausti Jónsson, 2000. ’Little Ice Age’ Research: A Perspective from Iceland. Climatic Change. 48 9-52. Páll Bergþórsson 1969a. An estimate /climatology/articles/nr/1138

• 27. Early work and an overview of measurements

  for more than 80 years in most parts of the country. Back to top Additional material and references: Trausti Jónsson og Hilmar Garðarsson 2001. Early Instrumental Meteorological Observations in Iceland. Climatic Change 48, 169-187. Ogilvie, A. E. J. og Trausti Jónsson, 2000. ’Little Ice Age’ Research: A Perspective from Iceland. Climatic Change. 48 9-52. Páll Bergþórsson 1969a. An estimate /climatology/articles/nr/1138/

• 28. Earthquakes offshore north Iceland

  offshore north Iceland 1.10.2013 Two earthquakes reaching magnitude 3 and 3.2 occurred this morning at 06:14 and 07:41 offshore North Iceland, 10 km NW of Gjögurtá. They are a part of swarm activity which has been ongoing since September 25. Roughly 1000 /about-imo/news/nr/2757

• 29. News

  October 2013 off shore North Iceland. Roughly 1000 earthquakes have been recorded in the swarm. Topography of seabed: Bryndís Brandsdóttir, Institute of Earth Sciences, University of Iceland. News 2023 2022 2021 2020 2019 2018 2017 /about-imo/news/bigimg/2757

• 30. tj_hofsj-langj-ces2010-video

  Year: 1990 Year: 1995 Year: 2000 Year: 2005 Year: 2010 Year: 2015 Year: 2020 Year: 2025 Year: 2030 Year: 2035 Year: 2040 Year: 2045 Year: 2050 Year: 2055 Year: 2060 Year: 2070 Year: 2075 Year: 2080 Year: 2085 Year: 2090 Year: 2095 Year: 2100 Year: 2100 /media/vedurstofan/utgafa/hlidarefni/tj_hofsj-langj-ces2010-video.pdf