).
Such crustal movements are very rapid over large areas in Iceland, particularly
in the southeastern part of the country. This type of analysis has now been
carried out for the Icelandic glaciers in a collaboration between scientists at
the Danish Space Institute (DTU-Space) and Icelandic glaciologists as a part of
the Nordic Centre of Excellence SVALI . The results are in agreement with the rapid
/about-imo/news/the-icelandic-glaciers-weighed-from-space
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Lidar measurements
of the cryosphere
Reykholt, Iceland, June 20–21, 2013
Abstract volume
Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland,
surveyed by TopScan GmbH in August 2011
Lidar measurements of the cryosphere
/media/vatnafar/joklar/Reykholt-abstracts.pdf
understanding of the problem may only
be reached by stakeholder dialogues.
2.1.2 Type of Uncertainty
Walker et al. (2003) distinguished between various levels of uncertainty: determinism,
statistical uncertainty, scenario uncertainty, recognised ignorance and total (unrecognised)
ignorance. Refsgaard et al. (2007) added qualitative uncertainty from Brown (2004) and
adopted the name ‘types’ instead
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
system ................................................. 21
Figure 6: Map of Heimaey showing the regular, gridded locations where modelled lava flows
originated ................................................................................................................................. 25
Figure 7: Modeled extent and thickness of lava from Small, Moderate, and Large eruptions
originating from
/media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
been rather intensive over the last 24 hours. Yesterday 13 earthquakes larger then M3,0 were
detected in Bardarbunga. The biggest was M5,2 at 18:09 last night. In total 7 earthquakes larger then M3,0 were
detected since noon yesterday. Smaller earthquakes were detected in Dyngjujokull glacier and in north part of the
dyke.
GPS monitoring continue to show irregularity in in the crustal
/media/jar/Factsheet_Bardarbunga_20140918.pdf
The lava flow is now around the centre of the lava
field, which is now around 37 square kilometres. According to new measurements the total volume of the lava is
0,4-0,6 cubic kilometres and the magma flow 250-350 cubic meters pr. second.
The subsidence of the Bardarbunga caldera continues with same rate as before.
Big earthquakes are still detected in the Bardarbunga caldera. Since noon
/media/jar/myndsafn/Factsheet_Bardarbunga_20140922.pdf
in Iceland: Climate projections and historical changes in precipitation type Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Halldór Björnsson, Matthew J. Roberts & Tinna Þórarinsdóttir99
20,6
/about-imo/publications/2022/
Exploratory and normative scenario developers both have acknowledged the added
value of either type of scenario process. Particularly the backcasting community has attempted to combine backcasting and
foresighting approaches. Good examples are Robinson et al. [10], Carlsson-Kanyama et al. [11], and the work of David Banister (e.g.
[12]). In this paper we describe an attempt from the community
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf