meteorological services for large areas of the North Atlantic and Green-
land. It is the second largest aviation service region in the world. Over the course of a decade IMO was modernized
and sta?ed to meet the highest international requirements. The Icelandic public and economic sectors, in particular
the fisheries, transportation and agriculture, benefitted hugely from this development making
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
the
interior of the ice sheet is somewhat too dry (Fig. 9b). By average a mean negative precipitation
bias of 0.16myr−1 results which equals 43% of the mean from Burgess et al. (2010) (Table 2).
6 Bias Correction and Future Scenario Runs
After having specified a number of biases in the RCM output the model runs were repeated
with bias-corrected RCM data.
To correct the temporal bias of Ta, daily
/media/ces/ces_geus_paakitsoq_full_report.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.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
tg
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aint
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incorp
orated
:
1:
Ep
ist
/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
the report.
2 Study area and data
2.1 River basins
The region under study is located in the East fjords and the surrounding area (Fig. 1). This region
is characterised by a complex topography along the coast, Vatnajökull ice cap in the southwest
and highlands in the interior. This leads to large precipitation and temperature gradients in the
region (Crochet et al., 2007; Crochet & Jóhannesson, 2011). Eight
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.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