by 25 % in the interior of Ice-
land, where the large ice caps are located (Nawri and Björns-
son, 2010).
Before year 2010, the glacier model is forced with daily
mean records constructed from the monthly mean observed
temperature and precipitation as previously explained. Pos-
sible natural variations in the climate are important for near-
future projections as the magnitude of the expected
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
Kjøllmoenet al. 2007).Storbreen is located just east of the main waterdivide between east and west in southern Norwayand receives precipitation from both directions(Liestøl 1967). The glacier is part of an east–west
mass balance transect in southern Norway where
mass turnover is largest near the western coast anddecreases towards the drier interior (Andreassen etal. 2005). Storbreen is in this respect
/media/ces/GA_2009_91A_4_Andreassen.pdf
the analysis will allow us to present the
outline for a new, potentially more robust and
comprehensive design process. The outline as
presented here consists of principles, phases and
their interior steps, and tools for participation
processes.
We will now turn to the various elements of the
potential new guide. We will start by presenting the
principles of design, followed by the steps and tools
/media/loftslag/vonKorff_etal-2010.pdf
site.
No changes have been made to the restricted area north of Vatnajökull.
The Civil Protection still operates in alert phase.
Aviation Colour Code for Bárðarbunga has been downgraded from orange to yellow.
From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga has been downgraded from orange
to yellow. The Aviation Colour Code system for Icelandic Volcanic
/media/jar/Factsheet_Bardarbunga_20150228.pdf