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of microearthquake activity south of lake
Hestvatn gave strong indications of where the next large earthquake would occur. A formal
warning was issued to the National Civil Protection Agency 26 hours prior to the ML 6.5
event which occurred on 21 June at 00:51:46.95 GMT. Its hypocentre was located at
63.98°N and 20.71°W and at a depth of 5.1 km. A preliminary estimation of the fault plane
based
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
is provided showing the number of lightning per hour in Iceland for
the past 24 hours (Fjöldi eldinga).
Also available is a table of lightning data for the past week (Eldingalisti). The list shows one
line for each located lightning in the area 63‒67°N, 13‒25°W, the latest data first. It includes
date and absolute time (UTC) of the lightning, a unique identification number (not really
useful
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
south of Vatnajökull as well as the south coast were monitored for gas pollution.
Volcanic gas dispersion was quite extensive. Almost no pollution was seen around Reykjavík during take off. Northeast of Þingvellir a white or light brown gas cloud became visible on top of the cloud cover, aggregating in the troughs. The gas seems to drift in bands or veils that are not continuous, with clean air
/earthquakes-and-volcanism/articles/nr/3011
south of Vatnajökull as well as the south coast were monitored for gas pollution.
Volcanic gas dispersion was quite extensive. Almost no pollution was seen around Reykjavík during take off. Northeast of Þingvellir a white or light brown gas cloud became visible on top of the cloud cover, aggregating in the troughs. The gas seems to drift in bands or veils that are not continuous, with clean air
/earthquakes-and-volcanism/articles/nr/3011/
) in their
definition of the relevance of scale, it is worthwhile
to check which types of scales as proposed by Cash
and his colleagues are used in the case study papers.
As can be seen in Table 1, all case studies explicitly
mention the importance of spatial scale, while
almost all case studies mention jurisdictional scale,
either explicitly or implicitly by giving importance
to, for example, the national scale
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
................................................................. 30
9
1 Abstract
Between 1991 and August 2006, 860 earthquakes in Eyjafjallajökull volcano, South
Iceland were recorded by the SIL national seismic network. These earthquakes have been
relocated using a relative, double-difference location method and their source mechanisms
recalculated. The spatial and temporal seismicity pattern is analysed, as well as the
distribution of focal
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
and web-based ash reports
from the public.
Eruption plume:
Height (a.s.l.): Mainly ~7 km / 24,000 ft.
Heading: West and later southwest.
Colour: Grey.
Tephra fallout: Ashfall reported from the Vestmanna Islands, Rangárþing east and in
Reykjavík.
Lightning: More than 50 lightning strikes were recorded on the ATDnet during the
last 24 hours. Between 4 and 5 this morning, 10 lightning were
/media/jar/Eyjafjallajokull_status_2010-05-14_IES_IMO.pdf
change has recently
been the subject of increased international attention, especially following the entry
into force of the Kyoto Protocol, the first step to globally reduce human influence on
the climate system. However, official national governmental responses to climate
change on the two sides of the Atlantic have been very different. The European
Union (EU) politically has been a fervent supporter
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
management actions. Stakeholder participation in
water-planning and management processes is
equally driven by supranational directives such as
the European Union (EU)’s Water Framework
Directive (EU 2000, 2002), national policies such
as the Australian National Water Initiative (Council
of Australian Governments 2004), and championed
as a key underlying principle in integrated water
resources management
/media/loftslag/Moellenkampetal_etal-2010.pdf