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systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com-
bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement
compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or
better than persistence, depending on catchment and lead time. Usually, persistence performs
better for T=1 day and then method 3
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
the com-
plexity of the hydrological processes through modelling, but its application is usually limited to
the short-range. Although the results demonstrated a great potential for this method, its success-
ful application in real-time will strongly depend on the quality and availability of streamflow
observations, which can be poor or simply missing during periods of variable durations, e.g
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.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
)
is shown. At the margin the grid boxes of the RCAO RCM are
visible. The area between Illulisat and Swiss camp is commonly
called Paakitsôq.
respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located
on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and
Box, 2001). The locations of the stations are indicated in Fig. 1, further details
/media/ces/ces_geus_paakitsoq_full_report.pdf
and water, „we are the only country with
the word „ice“ in its name. I welcome you all, in particular those who have
come from abroad. I hope you have a nice time here in Iceland. I hope you will
feel the warmth here – even though there is little or no volcanic activity
going on as we speak, and even though we worry about a warming world. There is
good warmth and there is bad warmth“ Mr
/about-imo/news/we-need-to-control-our-footprint-on-mother-earth
operational cost, etc.) and the annual
revenues
• consider an appropriate discount rate and assess NPV (net present
value), IRR (internal rate of return), and net cash flows
• rank alternatives by score level
• SCBA: social CBA – total benefits -/- total costs for society, in this
case benefits and costs often don’t accrue (entirely) to the same
organisation due to the public nature of a project
/media/loftslag/Perrels-CBA.pdf
acceptance, we
request a copy of the final manuscript, and as
many figures as possible, on a computer
diskette. It is essential that the name and
version of the word processing program and
computer type, is included on the diskette.
Preferred software formats are LaTex or MS
Word. The editors also welcome an ascii-text
version of the final manuscript in electronic
mail. Short to moderate
/media/jar/Jokull-guidlines.pdf
www.nordicadaptation2014.net
SCOPE
Welcome to the Third Nordic International Conference on Climate Change Adaptation. The
conference is a follow-up to the highly successful conferences in Stockholm (2010) and Hel-
sinki (2012) and aims to bring together scientists, practitioners and policy-makers with a par-
ticular interest in the Nordic region.
Please note that early bird registration
/media/loftslag/myndasafn/Nordic_Adaption_14_2cir.pdf