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• 61. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 62. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 63. Reports and publications

  et al. 3 2005 Seismic hazard in the Hengill area based on the SIL earthquake catalogue - First results (PDF) Kristján Ágústsson, Páll Halldórsson 42 0,8 2005 A model of the release of the two June 2000 earthquakes based on all available observations (PDF) Sigurlaug Hjaltadóttir, Kristín S. Vogfjörð, Þóra Árnadóttir, Páll Einarsson, Peter Suhadolc 8 8,2 2005 /earthquakes-and-volcanism/reports-and-publications/

• 64. Update on volcanic activity in Grímsvötn

  affecting the area around the crater. 26 May 2011 - 14:45 Yesterday, a group walked towards the eruptive site. Surveillance revealed much ash west and south of Grímsvötn. A few measurements, at locations where the ice was completely covered, gave ash thicknesses varying from 10 to 130 cm. Photo by Vilhjálmur Kjartansson, 25. maí 2011: 25 May 2011 - 18:05 Collective status report (pdf 35 Kb /earthquakes-and-volcanism/articles/nr/2180

• 65. Bardarbunga_kafli20140825

  have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf

• 66. ved-eng-2015

  stations was unusually small compared to the long term. Temperature anomaly °C (relative to 1961 - 1990) Figure 1. In Akureyri (red) the temperature was above the 1961-1990 mean during the first four months and again in the autumn; September was particularly warm, but May and August very cold. In Reykjavík (blue) May was very cold, but September warm. The absolute maximum temperature /media/vedurstofan/utgafa/skylduskil/ved-eng-2015.pdf

• 67. The weather in Iceland 2015

  in the Southwest. The weather in December was stormy. The year 2015 was the coldest in Iceland since 2000, but this period has generally been abnormally warm so the average temperature was close to the 1961-1990 mean. In most parts of the country the precipitation was well above normal. Temperature The average temperature in Reykjavík was 4.5°C, 0.2°C above the 1961-1990 mean. This is the 20th /about-imo/news/nr/3273

• 68. Markarfljót outwash plain and Öræfajökull

  was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company. Published material Under the link below, each of the chapters can be downloaded or short summaries read. Pagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 69. Factsheet_Bardarbunga_20150130

  ), to the east (middle) and vertical (bottom) in mm. Background signals have been removed from the time series. From May 2014 a displacement to North-West is detectable, which may be connected to the tension in Bardarbunga. Displacement towards the Bardarbunga caldera can be detected on the 16th of August (blue line), when the seismic activity started. A disturbance in the signal is detected /media/jar/Factsheet_Bardarbunga_20150130.pdf

• 70. VI_2013_008

  on the use of analogues. Analogue-based methods have been used with success in streamflow forecasting. They are often referred to as nearest-neighbor methods (Karlsson & Yakowitz, 1987; Galeati, 1990; Akbari et al., 2011). The first step of the technique is to compare a current situation to all past situations collected in an historical archive, according to a set of attributes describing /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf