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• 51. bb100days_ens

  ). These numbers could be compared with the largest gas-rich eruption occurred in Iceland in 1783-1784 (Laki eruption) and lasted 8 months. It has been estimated that during that eruption up to 122 Mt of SO2 were released into the atmosphere. Assuming a constant gas flux during the 8 months, the Laki eruption injected ~51 Mt in 100 days (5 - 15 times the Holuhraun‘s amount). /media/jar/bb100days_ens.pdf

• 52. Factsheet_Bardarbunga_20141015

  greater than M3.0 were recorded over the last 48 hours in or around the caldera. The largest one were M4.8 at 18:51 yesterday.  Little seismic activity is now detected in the northern part of the dyke and around the eruption site.  GPS measurements show minor movements. No great changes were detected.  No change was detected in water monitoring that cannot be explained by changing weather /media/jar/Factsheet_Bardarbunga_20141015.pdf

• 53. Factsheet_Bardarbunga_20141027

  is increasing in Bardarbunga. A cauldron in the southeast corner of Bardarbunga has deepened about 25 meters over a one month period. The depression is considered to be linked to the depression of the Bardarbunga caldera.  Over 70 smaller earthquakes are detected in the dyke over the weekend. The biggest was M2.1 at 11:51 on Sunday.  GPS measurements in the active area show minor changes /media/jar/Factsheet_Bardarbunga_20141027.pdf

• 54. Factsheet_Bardarbunga_20141119

  in the crater to east southeast.  Seismic activity in Bardarbunga continues to be strong. The two biggest earthquakes that were detected since noon on Monday were both of magnitude M4,6. On Tuesday, 18. November at 18:21 and on tonight, 19. November, at 00:29. In total 16 earthquakes bigger then M4,0 were detected over the period and 51 earthquakes between M3,0- 3,9. In total 200 earthquakes were /media/jar/Factsheet_Bardarbunga_20141119.pdf

• 55. Factsheet_Bardarbunga_20141124

  to the earth’s surface than was estimated before.  On Saturday, 22 November, at 00:51 an earthquake of magnitude M1,7 was detected in the dyke. In total about 80 earthquakes were detected in the dyke and around the eruption site in Holuhraun since Friday.  The subsidence of the Bardarbunga caldera and tectonics continues with similar rate as last few weeks. Tectonics movements show /media/jar/Factsheet_Bardarbunga_20141124.pdf

• 56. Factsheet_Bardarbunga_20140922

  yesterday there have been 9 earthquakes bigger the M3,0. The biggest one was measured M5,5 at 10:51 yesterday morning making it the second biggest earthquake since this wave of seismic activity started on August 16. Smaller earthquakes were detected in north part of the dyke and around the eruption site.  Earthquakes up to M4 have been measured under the north-north-west mountain side /media/jar/myndsafn/Factsheet_Bardarbunga_20140922.pdf

• 57. The

  February, the total accumulation was 51 cm. This has only once been exceeded, in January of 1937 when the snow depth was 55 cm. There was not much snow in Akureyri in 2017. Snow covered the ground completely for 50 days, 52 fewer than on the average 1971 to 2000. Days with total snow cover have never been so few in Akureyri since snow cover observations started in 1924. The greatest /about-imo/news/the-weather-in-iceland-in-2017

• 58. Isskyrsla_20100407

  - W022°51' 12.N67°42' -W022°10' 13.N67°42'- W022°20' 14.N67°47' -W022°08' 15.N67°46'- W021°40' 16.N67°46' -W021°37' 17.N67°38' -W021°05' 18.N67°43' -W021°02' Næst landi: 52 sml NV af Barða. 48 sml NV af Straumnesi. Hér að neðan er nákvæm staðsettning ísjaðarsins ________________________ Friðrik Höskuldsson Yfirstýrimaður 1. N65°49.46' W028°04.81' 2. N65°44.19' W027°49.00' 3. N65°42.85' W027°38.41 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 59. Keranen_Jaana_CES_2010

  erations which will be done to protect against th e phenome na a nd its conse quenc es The consequenc es of the phenom ena to the distribution network T he con seque nc es of the phe nom ena to the pow er plant The conse quence s of the phe nomena to e nerg y sourc e and its usability Probability according to IP CC 2007 Phe nom ena acco rding to regional scena rio /media/ces/Keranen_Jaana_CES_2010.pdf

• 60. Hydropower, Hydrology

  management, XXVI Nordic hydrological conference, Riga, Latvia August 9-11 2010. Nordic hydrological programme report No. 51. p138-139. Kurpniece. L., Lizuma, L., Timuhins, A., KolcovaT., Kukuls, I. (2010). Climate Change Impacts on Hydrological Regime in Latvia. Conference on Future Climate and Renewable Energy, Oslo, May 31-June 2, 2010. Meilutytė-Barauskienė D., Kriaučiūnienė J. & Kovalenkovienė M /ces/publications/nr/1938