stakeholders throughout the participation
process. This reflection should be based on
the stakeholders’ levels of interest, their
expertise and influence, and the objectives of
the process.
6. SA 6: Prepare for potential issues and
concerns. Try to foresee any issues that may
come up in the discussions with the
stakeholders so that preparatory work such as
studies, policy decisions, and information
/media/loftslag/vonKorff_etal-2010.pdf
reported
Most notices come from regions where avalanche observers work
Number of avalanches:
Size 1 and 1,5:
Size 2 and 2,5:
Size 3 and 3,5:
Size 4 and bigger:
Total
/avalanches/notifications/
; Ahlmann
and Thorarinsson, 1943; Thorarinsson, 1939, 1943).
The glacier was revisited in 2001 when the surface and
bed topographies were mapped. In 2002, automatic weather
stations were placed at 2 locations on the glacier and a still
ongoing surface mass balance survey was initiated. In addi-
Fig. 1. (A) Iceland and the largest ice caps, Vatnajökull (Va),
Hofsjökull (Ho) and Langjökull (La/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
The eruption has come to an end
The volcanic eruption in Holuhraun lasted six months
15.3.2015
The volcanic eruption in Holuhraun has come to an END, see a declaration from the Scientific Advisory Board, 28 February 2015.
For the first time in six months
/about-imo/news/nr/3097
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
Notes
The volcanic eruption in Holuhraun, which began on August 31st 2014, has come to an end.
The area continues to be closely monitored.
Gas contamination is still detected around the eruption
/media/jar/Factsheet_Bardarbunga_20150228.pdf
Reykjavı´k IS-101, Iceland
2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de
Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France
3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark
Keywords
Remote sensing; glacier mass balance;
regional warming
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
not determined in this study but it was suggested that they
might come from the large debris piles in the Efri-Botnar area.
Table 1. Age of the landslides according to 14C dating and observations of dated tephra
layers (Óskar Knudsen & Guðrún Larsen, 2014).
Landslide Uncorrected age (BP) Corrected age (AD, 1s) Corrected age (AD, 2s)
A 1286 38 670–770 650–820
B 1386 37 620–665 580–690
C 4500 – –
Table
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf