). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
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/media/loftslag/Guidelines2-for-rapporteurs.pdf
the average of the (wind speed) distribu-
tion is given by
m = AG(1+1=k) ; (2)
with gamma function, G, defined as usual. Wind power density, a measure of the energy flux
through an area perpendicular to the direction of motion, varies not only with the cube of wind
15
Figure 2. Annual modelled distributions (dashed lines) and corresponding Weibull fits
(solid lines) of wind speed at 50 mAGL, for two
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
lying areas in the City is illustrated for present climate in Figure 5. It is
expected that the future water level of the Horsens fiord will increase by 1 meter by the end of this
century.
Station 270045: Upstream Lake Nørrestrand
0
0.5
1
1.5
2
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3
3.5
4
1 2 3 4 5 6 7 8 9 10 11 12
Month
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Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
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2
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6
/media/loftslag/Horsens_case.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
opportunity evaluation
Case studies
NOE Net
SEAS-NVE
Findings of case studies
• Distribution companies generally well
equipped for climate change
– Cabling of all overhead lines well under way
– Distribution boxes in areas with increased risk of
flooding are elevated already
– Salt spray further inland is becoming an increasing
problem for substations and transformers
Cabling in Denmark
/media/ces/James-Smith_Edward_CES_2010.pdf
identified prior to the onslaught was the area coverage by weather radars. The northern
part of the country is not covered by weather radars: during these circumstances the weather came from the north
and was not observable by the present system.
The forecasting for the event was quite successful, and this is due in part to our strategy regarding international
and joint e?orts for weather
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
) and changing climate (CC:CC)
1. Current climate (CU)
- varying thinning regimes
(0%, 15%, 30%,45%)
2. Changing climate (CC)
- varying thinning regimes
(0%, 15%, 30%,45%)
3. Current (CU) &
changing climate (CC)
- current thinning regime
4. Current (CU) &
changing climate (CC)
- changed thinning regimes
C
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/media/ces/CES_BioFuels_Flyer_new.pdf
is N197°E. The J21 fault, on the other hand, is more
linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip
changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9
km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000
activity have also been mapped, including the fault planes of three M~5
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
of radiation are
added to a classic degree-day model. For infiltration, a methodology of Peschke, based on
the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated
soil zone, the Richards equation was used. The groundwater table was modelled in both the
unsaturated zone module and the groundwater module. The coupling between both modules
was done by a net/media/ces/2010_017.pdf