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Office, Institute of Earth
Sciences and Cambridge University confirmed the location of the eruption.
The eruption occurred on an old volcanic fissure on the Holuhraun lava field, about 5
km north of the Dyngjujökull ice margin. The active fissure was about 600 m in
length.
A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow
is thought to have stopped
/media/jar/Bardarbunga-2014_August-events.pdf
J. Roberts
Tinna Þórarinsdóttir
VÍ 2022-006
Skýrsla
+3 5 4 522 6000
vedur@ve d u r.i s
Veðursto f a Ísland s
B ú sta ð a rve g u r 7–9
108 Reyk j a vík
Contents
1 INTRODUCTION .................................................................................................................. 4
2 STUDY AREA
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length.
A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped.
According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC.
At the beginning of the eruption, seismic activity decreased, although seismicity has
/earthquakes-and-volcanism/articles/nr/3000
field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length.
A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped.
According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC.
At the beginning of the eruption, seismic activity decreased, although seismicity has
/earthquakes-and-volcanism/articles/nr/3000/
NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
1
Outline for the case Road maintenance in a changing climate
Introduction
Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and
Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary
5
• Conflict resolution mechanisms. The water sector is characterised by many strong
stakeholders, who have to compromise to allow a water management solution to be
achieved, and often the stakeholders are directly involved in negotiating the
management solutions. The national road sector decisions are more often made at the
central
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
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
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