In combination, the monthly articles give an overview of events: August, September,
October, November, December, January, February and the current update.
Calendar
Below is a calendar with a short-cut to each day of this month's events:
Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30
Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo
/media/jar/Bardarbunga-2014_September-events.pdf
February, March-April-May and the overview article (list of links).
Calendar
Below is a calendar with a short-cut to each day of this month's events:
Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30
Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo: Richard Yeo.
Updated information
30 September 2014 18:50 - from
/earthquakes-and-volcanism/articles/nr/3001
February, March-April-May and the overview article (list of links).
Calendar
Below is a calendar with a short-cut to each day of this month's events:
Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30
Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo: Richard Yeo.
Updated information
30 September 2014 18:50 - from
/earthquakes-and-volcanism/articles/nr/3001/
of
catchments (e.g. size, location, lake percentage) and (4) to evaluate
the usefulness of continental scale hydrological scenarios on a na-
tional scale in a country with variable hydrological conditions. The
results can be utilized in preliminary flood risk evaluation required
by EU Floods Directive, when lowest building elevation, flood risk
areas and flood adaptation options are planned
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
+ 1 is calculated for every time-step and over each grid
cell of the DTM according to Oerlemans (2001):
bc(t+ 1) = bc(t) +
braceleftBigg
∆t · (−Qm)/lm + Psolid if Qm > 0
Psolid if Qm ≤ 0
(1)
where t is the discrete time variable, ∆t is the time-step, lm is the latent heat of fusion of ice
(334 kJ kg−1) and Psolid is solid precipitation in meter water equivalent (m w.e.). The energy
available
/media/ces/ces_geus_paakitsoq_full_report.pdf
an operational monitoring system exists
to track ash dispersion.The monitoring network around Katla volcano is dense. Seismic stations
are marked as black triangles (SIL-stations). Missing from the map are
gas-sensors at Sólheimaheiði and Sólheimajökull, a bore-hole strain meter at
Eystri-Skógar and other instruments farther away, which are also significant
for volcano monitoring, e.g. infrasound
/about-imo/news/100-years-since-katla-erupted
On the northern side a tephra wall rises 20 meters above the water. The ice walls at the southwestern corner of the crater are melting, i.e. at the site of the vent that was active 4 - 6 June. The rate of melting is assumed to be about one cubic meter per second.
Details on the volume of the lake, and possible flooding from it, in a status report issued collectively by the Icelandic Meteorological
/earthquakes-and-volcanism/articles/nr/1884