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/weather/stations/
meðallagi á árinu. Mikið norðanóveður gekk yfir landið dagana 10. til 11. desember sem
olli miklu tjóni. Verst var veðrið á Ströndum, Norðurlandi vestra og Norðurlandi eystra. Mikil ísing og fannfergi fylgdu
óveðrinu sem olli því að hundrað hross fennti í kaf, skemmdir urðu á rafmagnslínum með tilheyrandi rafmagnstruflun-
um og mikil röskun varð á samgöngum.
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/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
Berthier3
1Institute of Earth Sciences, University of Iceland
2The Icelandic Meteorological Office
3Centre National de la Recherche Scientifique, Laboratoire d’Etudes en Géophysique et Océanographie
Spatiale, Université de Toulouse, France
* Corresponding author, e-mail: sg (at) hi.is
ABSTRACT
We assess the mass balance changes of the ~81 km2 Eyjafjallajökull ice cap in South Iceland,
over three
/media/vatnafar/joklar/Reykholt-abstracts.pdf
global climate models. The
numbers in the top left corner give the probabilities of very cold (below the 10th percentile in
1961-1990, threshold shown by the first vertical line), cold (below the 50th percentile, second
vertical line), warm (above the 50th percentile) and very warm (above the 90th percentile,
third vertical line) Decembers for 1961-1990, 1961-2008 and 2010.
To quantify
/media/ces/CES_D2.4_task1.pdf
12. On a photograph from 2003 there is little or no evidence of the fracture, however, in 2011 a clear fracture can be seen. Shortly before the rockslide, the material below the fracture seems to have sunk considerably. The crown of the rockslide is just above the fracture. Compiled by Jón Kristinn Helgason.
Fig. 13
Figure 13. Fractures in the snow could be seen days before
/avalanches/articles/nr/2929
for the hydrological year 1980 – 1981 (Figure 4, top), the method
works well. The date retrieved corresponds exactly to the moment the snowpack starts
decreasing continuously, and a steep increase in the melting line can be noted, indicating the
onset of the melt season. However, this filter does not work in all cases, as shown for
Hágöngulón for the years 1986 – 1987 (Figure 4, bottom). In that case
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf
and in the uppermost rows of houses below Botnabrún. The
most effective mitigation options to improve the landslide hazard situation in southern
Seyðisfjörður is draining of the main source areas in Neðri-Botnar in the lower part of the
mountainside as well as a construction of a moderately high catching dam above the top
row of houses below Botnabrún, and debris retention basins and guiding dams at the
lateral
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf