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• 41. Bárðarbunga 2014 - October events

  The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011

• 42. Bardarbunga-2014_October-events

  previously been observed for several M>5 events and can not be interpreted as a decrease of the overall activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part /media/jar/Bardarbunga-2014_October-events.pdf

• 43. Bárðarbunga 2014 - October events

  The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011/

• 44. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 45. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 46. CES_D2_2_poster_3x3

  (median) changes from the model-based hindcast. Bottom: the location of the observed change within the hindcast probability distribution. Blue (red) shading indicates areas where the observed change was above the 95th percentile (below the 5th percentile) of the hindcast distribution. These maps show that there was no detailed agreement between the best-estimate precipitation change hindcast /media/ces/CES_D2_2_poster_3x3.pdf

• 47. Summary of activity in Bárðarbunga

  and will update in case of any changes. Manually checked earthquakes Fig. 1. All manually checked earthquakes since the beginning of the sequence. Event times are colour coded, events larger than magnitude 3 are given as green stars. The migration of the activity from the caldera of Bárðarbunga (dark blue, Saturday) to the northern and eastern clusters (light blue, Sunday; orange Monday) can be seen /about-imo/news/nr/2942

• 48. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 49. Bardarbunga_daily_status_report_22082014

  Bárðarbunga update 22082014 2014-08-22 16:37 UTC Bárðarbunga update Compiled by Melissa Anne Pfeffer Sara Barsotti Hildur María Friðriksdóttir Bergþóra Þorbjarnardóttir Bergur Einarsson Þóra Árnadóttir Ásta Rut Hjartardóttir Michelle Parks Based on Seismic, GPS, water samples Eruption plume Height (a.s.l.) No eruption and no eruption cloud. Heading No eruption and no eruption cloud. Colour /media/jar/Bardarbunga_daily_status_report_22082014.pdf

• 50. Bárðarbunga 2014 - December events

  (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist on duty Bárðarbunga: The largest earthquake measured the last 24 hours was M4.5 and occurred at 16:12 yesterday /earthquakes-and-volcanism/articles/nr/3055