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
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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
glacier, and a general land rise
along the southern coast and in the countries interior (figure 1). This rise results from recent melt
of the Icelandic glaciers, which have been melting since the late 19th century. An acceleration in
land uplift is even evident in the Southeast. STL analysis of vertical GPS measurements in 1997-
2015 from Höfn in Hornafjörður show over 8 mm/yr uplift in the first
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf