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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
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
N and 23°49'W.
No seaice was in the Greenland Strait in September. Northeasterly winds prevailed in the area in the beginning of the month but westlies in the last days
/sea-ice/monthly/2009/nr/2331
- 023°46´W.
Wind directions were mostly from the northeast but there were a few days of northerlies, easterlies and northwesterlies on the Greenland Strait
/sea-ice/monthly/2010/nr/2345
Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009
ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost
operating manage- ment develop- poned-, of land grants ons European tax over- level
costs ment ment comprehen- build- and com- Regional De- heads
1991- 1991- sive- and ings pensation
/media/loftslag/Traffc-maintenance_expenditures.pdf
0.501.05 12:17:2553.56.8 km NW of Grímsfjall
0.601.05 11:38:13Check.6.9 km NNW of Grímsfjall
0.301.05 11:36:41Check.7.7 km NE of Krýsuvík
0.701.05 11:31:58Check.4.6 km SE of Bárðarbunga
0.501.05 10:53:07Check.5.1 km S of Fagradalsfjall
1.001.05 09:20:04Check.3.1 km E of Flatey
0.501.05 08:53:41Check.4.8 km W of Þrengsli
0.901.05 08:35:09Check.2.4 km NE
/m/earthquakes/latest
and direction, as well as air temperature, from the IMO operational surface station net-
work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some
stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m.
3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary
data file: grib_set -f -d 0.0 -w/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf