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/
communication). The HIRHAM4 model run reaches from
1950–2100 and incorporates Greenland at a resolution of approx. 25km. Ahlstrøm et al. (2008a)
have analyzed its bias in air temperature and precipitation over the ice sheet at Paakitsôq,
Aðalgeirsdóttir et al. (2009) compared those two parameters to a larger number of weather
stations over Greenland.
3 Methods
3.1 Mass Balance Modeling
/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
............................................................................................................... 33
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
3
CryoSat-2 Arctic sea-ice freeboard and thickness data product and its validation
Ciaran Robb, Ian Willis and Neil Arnold ............................................................................ 34
Using airborne remote
/media/vatnafar/joklar/Reykholt-abstracts.pdf
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
· Climate change · Adaptation ·
Hydrological modelling · Impact assessment
1 Introduction
Climate change is predicted to affect the hydrology of Finland considerably. By the
2080s average annual temperature in Finland is expected to increase by 3–7◦C and
average precipitation by 13–26%, with the largest increases during winter (IPCC
2007; Ruosteenoja and Jylhä 2007). The hydrology of Finland
/media/ces/Water_resources_man_Veijalainen_etal.pdf
at midnight on the 6th of April and is between the
two existing fissures. Rescue teams from the Icelandic Association for Search
and Rescue had detected subsidence in the area on the 6th of April about
420 meters northeast of the original eruption area in Geldingadalir, which was
about 150m long and about 1 meter deep. In the photos that were taken
during the reconnaissance flight on the 7th
/about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir