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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
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
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
). Distribution of snow accumulation on the Svartisen ice cap, Norway, assessed by a model of orographic precipitation. Hydrological Processes, 22(19), 3998-400.
Other international
Crochet, P., Jóhannesson, T., Sigurðsson, O., Björnsson, H. & Pálsson, F. (2008). Modeling precipitation over complex terrain in Iceland. In: Sveinsson, Ó. G. B., S. M. Garðarsson and S. Gunnlaugsdóttir (eds.), Northern
/ces/publications/nr/1940
was chosen because after 1980 sea ice is fully initiated in RCAO
and after 2006 the records from the weather-stations end. (The stations actually continue to
4
Figure 2: mass balance profiles calculated using RCAO (Plot a) and
HIRHAM4 (Plot b) for model input.
measure, but in the short time available for the Paakitsoq mass balance project we did not
look for more data.) The reference period
/media/ces/ces_geus_paakitsoq_full_report.pdf
3. Differences in terrain elevation between HARMONIE model and 100-m-
resolution DEM (model minus DEM): (a) original DEM interpolated onto the HAR-
MONIE model grid, and (b) DEM horizontally averaged around each model grid point,
using an exponential shape function with a half-width of 1 km.
In addition to surface type, boundary-layer atmospheric properties are strongly influenced by
the height
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
are listed in Table 12.
Table 11. Hypotheses in Table 12 explained.
Hypothesis
A There is more warming in the north of Iceland
B There will be more warming in winter than in summer
C The total precipitation amount will increase
D The wind speed will decrease in the future
Table 12. The hypotheses in Table 11 compared to the findings of our study and six
others. A question mark (?) indicates
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
from October 5, 2004
- spatial resolution: 40x40 m
- accuracy: 10 m in elevation and 30 m in horizontal position
b) SPOT 5 HRS from August 14, 2004
c) EMISAR from August 12, 1998
- reference map for co-registration and offset correction
- spatial resolution 5x5 m
- accuracy <2 m in elevation and 5 m in horizontal position
d) aerial photographs from the 1980s:
i. Torfajökull ice cap (To) from
/media/ces/glacier_mass_balance_poster.pdf
Swe). CLIMATOOL
12:15 - 13:15 lunch
13:15 p6 Rolf Johnsen (Region Midt, Dk). Climate change adaptation - Collaboration and innovation in society, science and industry is needed
13:45 - 15:15 parallel break-out sessions:
Case A: Local but comprehensive case: Horsens fjord - Introduction by Jes Pedersen
Case B: Road infrastructure planning & operation case - Introduction Heikki Tuomenvirta
/nonam/workshop/program/