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Figure 1. Scenario building for AWM in Horsens Fjord
To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments
of the productivity of this approach are based on main big strategies which need to have an attention.
One of them
/media/loftslag/Group-1_Scenarios-for-AWM.pdf
in an overall
cold bias, compared with station measurements. To test, whether this is due to the HARMONIE
model core or the external surface scheme, biases of 2-m temperature from SURFEX are com-
pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is
found that the negative temperature biases are due to shallow inversion layers near the ground,
which are introduced
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
). Locations of the weather sta-
tions, used to reconstruct the temperature and precipitation records,
are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H),
Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri
(A) and Hólar in Hornafjörður (HH). (B) The surface topography of
Vatnajökull ice cap. Dots show the sites of mass balance and veloc-
ity measurements, blue dots show
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
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/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
Radic, V., Roald, L. A., Rosberg, J., Rogozova, S., Sigurðsson, O., Suomalainen, M., Thorsteinsson, T., Vehviläinen, B., & Veijalainen, N. (2007). Impacts of climate change on river runoff, glaciers and hydropower in the Nordic area. Joint final report from the CE Hydrological Models and Snow and Ice Groups. Reykjavík: Climate and Energy [Report (high resolution 15 MB)] [Report (low resolution 4 MB
/climatology/research/ce/publications/
: to use or not to use?
*O'Neill, R. V., and A. W. King. 1998, Homage to St. Michael; or, why are there so
many books on scale?: Pages 3–15 in D. L. Peterson and V. T. Parker (editors).
Ecological scale: theory and applications. Columbia University Press, New York.
• Robert O’Neill questions the unifying capabilities*
• Aspects of the land use system have different scale properties
• To use
/media/loftslag/Kok_1-scenarios-lecture-1.pdf
Refsgaard a,*, Jeroen P. v
Peter A. Vanroll
a Geological Survey of Denmark and Greenlan
b Copernicus Institute for Sustainable Development and Innovation
Utrecht University, Utrecht
c
Environmental Modelling & Softwar
equitable manner without compromising the sustainability of
* Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050.
E-mail address: jcr@geus.dk (J.C. Refsgaard).
1364-8152
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
This is also the case with
cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected
by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are
cyclones in the neighbouring sector, in which case pressure tendencies are reversed.
21
Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com-
posite mean
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
61, 1-18.
Oddur Sigurðsson (2011). Iceland glaciers. Í: V. P. Singh, P. Singh & U. K. Haritashya (ritstj.). Encyclopedia of Snow, Ice and Glaciers. Springer, Dordrecht, s. 630-636.
Árni Snorrason, Jórunn Harðardóttir & Þorsteinn Þorsteinsson (2011). Climate and Energy Systems – Project Structure. In: Þorsteinn Þorsteinsson & Halldór Björnsson (eds.), Climate Change and Energy Systems. Impacts
/about-imo/arctic/completed-projects/publications/