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• 71. Bárðarbunga 2014 - November events

  and another five between 3 and 4. Only five earthquakes occurred at the northern part of the intrusion, all under 1.5 in magnitude. 5 November 2014 - photos from flight Visibility was good during surveillance flight yesterday, 4 November, with almost no wind. The gas cloud was two layered, from the ground to 700 m hight and in about 1500-2500 m hight. Two layers of gas Visible distinction /earthquakes-and-volcanism/articles/nr/3023

• 72. Bardarbunga-2014_November-events

  November, with almost no wind. The gas cloud was two layered, from the ground to 700 m hight and in about 1500-2500 m hight. Two layers of gas Visible distinction as Mountain Herðubreið rises tall from the lower layer but is crowned by the upper layer. Enlarge. Photo: Guðrún Nína Petersen. Steam vents Steam vents rise from the lava field: water vapor. Gas further. Photo: Guðrún Nína Petersen /media/jar/Bardarbunga-2014_November-events.pdf

• 73. Bárðarbunga 2014 - November events

  and another five between 3 and 4. Only five earthquakes occurred at the northern part of the intrusion, all under 1.5 in magnitude. 5 November 2014 - photos from flight Visibility was good during surveillance flight yesterday, 4 November, with almost no wind. The gas cloud was two layered, from the ground to 700 m hight and in about 1500-2500 m hight. Two layers of gas Visible distinction /earthquakes-and-volcanism/articles/nr/3023/

• 74. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 75. Update on activity in Eyjafjallajökull 2010

  at Fljótshlíð, 10-15 km NW of vents. Meltwater discharge suggest similar lava activity. Processing of data obtained yesterday shows that lava had advanced 400-500 m northwards from crater, forming an ice depression extending some 700 m from vents. Overall assessment: Magma flow rate has remained at similar level over the last few days while plume activity is slowly declining. Lava continues /earthquakes-and-volcanism/articles/nr/1884

• 76. Bárðarbunga 2014 - September events

  indicate 200-600 kg/s SO2 over the last week of the eruption. Relating SO2 to other gases measured by FTIR preliminarily indicates 250-700 kg/s CO2, 2-6 kg/s HCl, 3-8 kg/s HF, and <1 kg/s CO. These emission rates may be underdetections due to measurement conditions. Experiments will be made this week to help us constrain the measurement bias and uncertainty, and these emission rates will likely /earthquakes-and-volcanism/articles/nr/3001

• 77. Bardarbunga-2014_September-events

  - gas emission rates Measurements of SO2 emission rates with permanently installed scanning DOAS instruments preliminarily indicate 200-600 kg/s SO2 over the last week of the eruption. Relating SO2 to other gases measured by FTIR preliminarily indicates 250-700 kg/s CO2, 2-6 kg/s HCl, 3-8 kg/s HF, and <1 kg/s CO. These emission rates may be underdetections due to measurement conditions /media/jar/Bardarbunga-2014_September-events.pdf

• 78. Bárðarbunga 2014 - September events

  indicate 200-600 kg/s SO2 over the last week of the eruption. Relating SO2 to other gases measured by FTIR preliminarily indicates 250-700 kg/s CO2, 2-6 kg/s HCl, 3-8 kg/s HF, and <1 kg/s CO. These emission rates may be underdetections due to measurement conditions. Experiments will be made this week to help us constrain the measurement bias and uncertainty, and these emission rates will likely /earthquakes-and-volcanism/articles/nr/3001/

• 79. VI_arsskyrsla2020

  /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf