few weeks before the eruption started and since then the stations is
showing a slow southwest movement which reflect a slow deflation process (Graph:
Benedikt Gunnar Ófeigsson). B) Shows where the magma intrution had formed
(Figure: IMO).Shortly
before the eruption onset the seismic activity decreased, and no earthquake over
M4 has been measure since. On the 19th of March at 20:45 the magma
/about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/
Extreme precipitation in Iceland: Climate
projections and historical changes in
precipitation type
Andréa-Giorgio R. Massad
Guðrún Nína Petersen
Halldór Björnsson
Matthew J. Roberts
Tinna Þórarinsdóttir
VÍ 2022-006
Skýrsla
Extreme precipitation in Iceland: Climate
projections and historical changes in
precipitation type
Andréa-Giorgio R. Massad
Guðrún Nína Petersen
Halldór Björnsson
Matthew
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
boundary flux between the unsaturated zone and the groundwater (Schulla
& Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each watershed by comparison of modelled and
measured discharge series.
In this study
/media/ces/2010_017.pdf
.............................................................. 41
Catching dams and debris retention basins below Botnabrún ........................... 41
Real-time monitoring and warnings ........................................................... 45
7.4 Protection measures for the Þófi area .......................................................... 45
Drainage ditches, retention basin and discharge pipes on Þófi .......................... 45
Point
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
the eastern half of the craters was measured and found to be up to 40 m thick. Intense steam rises up from the craters, with occasional small ashy explosions. The noise of intense boiling and or degassing is heard from the craters. The crater rim is coated with fine ash that extends 20 m from the edge. Strong smell of sulfur around the craters.
At 20:45 the steam plume was measured to be at the altitude
/earthquakes-and-volcanism/articles/nr/1884
Hensch, B. Lund, Th. Árnadóttir, B. Brandsdóttir12:00
– 12:10 Closing remarks Kristín
S. Vogfjörð, Kristín Jónsdóttir, Martin Hensch12:10 – 13:45 Lunch
break 13:45 – 19:00 Fieldtrip to Reykjanes peninsula 13:45
is the departure time outside Grand Hotel Reykjavík!
We
need to start the trip on time to avoid ending
/norsem/norsem2016/program/thursday
of activity in Bárðarbunga
State of events on Monday evening
19.8.2014
Summary written 18th August at 20:45
Since the onset of the earthquake swarm at Bárðarbunga on Saturday morning 16th August 03:00am, around 2.600 earthquakes have been detected with the earthquake
/about-imo/news/nr/2942
the satellite Meteosat-10 was declared operational at 09:45 UTC on 21 January 2013, just over a year ago. Reference: Satellites, Meteosat-10, Channels/Products, NIR1.6, VIS0.8, VIS0.6.
News
2023
2022
2021
2020
2019
2018
2017
2016
/about-imo/news/bigimg/2832
of Bárðarbunga that was active during the first days
automatic automatically detected events in the around and north of Vatnajökull
checked manually revised events
last update: 17. February 2015, 16:45 UTC
/media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf