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The rate of the subsidence in Bárðarbunga caldera had decreased substantially. But that is not the whole story. Ice is
subsiding into the caldera with the effect that the GPS station does not show any changes. The estimated depression
of the rock foundation of the caldera, in the light of the ice subsidence, is about 5 cm per day. The flow of magma
from under Bárðarbunga is believed
/media/jar/Factsheet_Bardarbunga_20150220.pdf
University of Iceland along with
representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland.
Main points
Volcanic eruption in Holuhraun
Air quality
Scenarios
Notes
The volcanic eruption in Holuhraun continues with similar rate as last few days. The eruption does not seem to be
declining. The lava production continues with the same strength
/media/jar/Factsheet_Bardarbunga_20140921.pdf
University of Iceland along with
representatives from the Icelandic Civil Protection, the Environmental Agency of Iceland and the Directorate of
Health.
Main points
Volcanic eruption in Holuhraun
Air quality
Scenarios
Notes
The volcanic eruption in Holuhraun continues with similar rate as last few days. The eruption does not seem to be
declining. The lava field continues
/media/jar/Factsheet_Bardarbunga_20140925.pdf
quality:
Considerable sulphuric dioxide (SO2) pollution has been recorded widely around Iceland over the last few days. It is
believed that reduced energy in the volcanic plume may result in that the gas pollution does not reach the higher
layers of the atmosphere.
Today (Friday) eastern gales are forecast so gas pollution is expected mainly in W-Iceland. Tomorrow (Saturday) light
easterly
/media/jar/Factsheet_Bardarbunga_20141031.pdf
University of Iceland along with
representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland.
Main points
Volcanic eruption in Holuhraun
Air quality
Scenarios
Notes
The volcanic eruption in Holuhraun continues with similar rate as last few days. The eruption does not seem to be
declining. The lava production continues with the same strength
/media/jar/myndsafn/Factsheet_Bardarbunga_20140922.pdf
has increased as a result of the disappearance for a
number of years of eel-grass. North of Alrø Island, as a result of the construction of a causeway
connecting the island to the mainland, sedimentation of silt is taking place. In the past years the grazing
of the saltmarshes on Endelave has been reduced due to smaller numbers of grazing cattle. The taller
vegetation is negative for the birds
/media/loftslag/Horsens_case.pdf
can therefore be represented by quantitative
measures, for example, a range of values
calculated by various models, or by
qualitative statements, for example,
reflecting the judgement of a team of
experts.
} What is it?
}
How can it be
characterised?
Where does it
come from?
}
Nature of uncertainty
Epistemic uncertainty
• uncertainty due to imperfect knowledge
reducible by more data
/media/loftslag/Refsgaard_2-uncertainty.pdf
the plume during its ascent. Only the finer
fraction of the erupted material (what is called volcanic ash) will be
transported by the wind within a volcanic ash cloud.
How far a volcanic ash cloud can be transported
depends on the height of the eruption column, the size of the ash, the wind
circulation and the efficacy of the removal processes. When the ash plume is
within the troposphere
/volcanoes/volcanic-hazards/volcanic-emissions/
of Jutland is saltmarsh. Furthermore there are heaths, moors, meadows and deciduous forests. Since the
1930s sedimentation around the islands and shoals has increased as a result of the disappearance for a
number of years of eel-grass. North of Alrø Island, as a result of the construction of a causeway
connecting the island to the mainland, sedimentation of silt is taking place. In the past
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
of Jutland is saltmarsh. Furthermore there are heaths, moors, meadows and deciduous forests. Since the
1930s sedimentation around the islands and shoals has increased as a result of the disappearance for a
number of years of eel-grass. North of Alrø Island, as a result of the construction of a causeway
connecting the island to the mainland, sedimentation of silt is taking place. In the past
/media/loftslag/Case_A___Horsens_Fjord.pdf