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mode ................................................... 14
5 Errors associated with SURFEX .................................................................... 15
6 Statistical correction of model results .............................................................. 19
7 Original and corrected 2-m air temperature .................................................... 22
8 Original and corrected 10-m
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
........................................................................................................................... 3
Summary ............................................................................................................................... 4
Summary of the break-out sessions on road infrastructure ................................................... 6
Summary of the break-out sessions on Horsens case
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
in the data used in making the
decision and the factors are interlinked, all of which makes
the problem highly complex. The part of the net defined by
variables and links is relatively easily communicated to
stakeholders (Henriksen et al., 2007b). However the
tal Management 88 (2008) 1025–1036
quantitative part, with the conditional probability tables
(CPTs), the numbers, is the step where
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
automatically detected from midnight until now are 400.
27 August 2014 20:50 - info from a surveillance flight
Scientists from IES and IMO on a flight to Vatnajökull tonight discovered a row of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when. Heightened
/earthquakes-and-volcanism/articles/nr/3000
of 10-15 m
deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The
cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain
when. Heightened tremor level/volcanic tremor has not been observed on IMO's seismometers
at the moment. The new data is being examined.
A field trip earlier today
A new GPS station being mounted near
/media/jar/Bardarbunga-2014_August-events.pdf
automatically detected from midnight until now are 400.
27 August 2014 20:50 - info from a surveillance flight
Scientists from IES and IMO on a flight to Vatnajökull tonight discovered a row of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when. Heightened
/earthquakes-and-volcanism/articles/nr/3000/
for the hydropower catchments ............................................ 36
6 CONCLUSIONS .................................................................................................................. 41
BIBLIOGRAPHY ...................................................................................................................... 42
APPENDIX I. MELT SEASON ANALYSIS
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf