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mode ................................................... 14
5 Errors associated with SURFEX .................................................................... 15
6 Statistical correction of model results .............................................................. 19
7 Original and corrected 2-m air temperature .................................................... 22
8 Original and corrected 10-m
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
improving
management policies and practices by learning from the
outcomes of implemented management strategies. Partici-
patory integrated assessment is here a form of problem
structuring for identification of gaps, ambiguity and
multiple frames, confrontation, and integration of the
most divergent views with respect to a given problem
situation.
Additional methods and tools that AM require com/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
of the glaciers. An up to 8 m thick winter snow layer
was measured in the accumulation area (∼4 m w.e.). Ice melt
of up 10 m w.e. was measured in the lowest part of the ab-
lation zone in summer, and 2 m w.e. was melted during win-
ter. Taking into account ∼2 m of annual rainfall, the runoff
from this part of the glacier was estimated as ∼14 m w.e. per
year; a surprisingly high value (Ahlmann, 1939
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
regimes of
Number of flood and drought disasters in the past
decades per case study
0
2
4
6
8
10
12
1977-1986 1987-1996 1997-2006
Time period
Total number of flood and
drought disaster
s
Rivierenland
Alentejo
Upper Tisza - Hungary
Upper Tisza - Ukraine
Fig. 1 Number of reported flood and drought disasters in the past
decades in Rivierenland, Alentejo, Hungarian part of Upper Tisza,
and Ukrainian
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
the variations in the seasonal componentsof the mass balance;
– use the model to reconstruct the mass balanceprior to 1949;
– study the sensitivity of the model to differentmodel set ups and choices of parameters;
– and study the climate sensitivity of the glacierand implications of climate change on the massbalance.
SettingStorbreen (61°36' N, 8°8' E) is located in the Jotun-heimen mountain massif
/media/ces/GA_2009_91A_4_Andreassen.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
decade within the 2004–50
period, for the UKMO HadCM3, and the MPI ECHAM5-r3. . . . . . . . . . . . . 28
7 Mean annual surface air temperature and total precipitation during the 1961–90
control period, and linear trends within the 1958–2001 period, for the ERA-40
reanalyses. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29
8 Differences between the RCM and underlying
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to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
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