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Conference on Future Climate
and Renewable Energy:
Impacts, Risks and Adaptation
31 May - 2 June 2010
Soria Moria Hotel and Conference Center, Oslo, Norway
Conference proceedings
1
Conference proceedings
Future Climate and Renewable Energy: Impacts, Risks and Adaptation
31 May – 2 June 2010
Soria Moria Hotel and Conference Center, Oslo Norway
Published by: Norwegian Water
/media/ces/ces-oslo2010_proceedings.pdf
of how climate change will
impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources
and taking advantage of the local tempered climate for keeping the
supercomputer components cool, the running costs and CO2 footprint
will be kept to a minimum, saving tonnes of CO2 in line with the
four nations' efforts towards reaching Net/about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Summerschool Copenhagen 22-26 August 2011 2
Physical features and ecosystem
The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations
/media/loftslag/Horsens_case.pdf
(DGPS) equipment
in 2001. Continuous profiles, approximately 1 km apart,
were measured in the accumulation zone and a dense net-
work of point measurements were carried out in the abla-
tion zone. Digital Elevation Models (DEMs) of the surface
and bedrock were created from these data (Fig. 2; Björns-
son and Pálsson, 2004). The estimated errors are at most
1–5 m (bias less than 1 m) for the surface
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
lidar surveys
Joaquín Muñoz-Cobo Belart, Eyjólfur Magnússon and Finnur Pálsson .......................... 11
Mass balance analysis of Drangajökull ice cap from historical photogrammetry and lidar
Beata Csatho, Thorsten Markus and Thomas Neumann ................................................... 12
The ICESat-2 mission: design, applications and pre-launch performance assessments
/media/vatnafar/joklar/Reykholt-abstracts.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
in sea surface level in the North Sea/Baltic Sea system
whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2
Physical features and ecosystem
The fjord landscape
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
in sea surface level in the North Sea/Baltic Sea system
whereas changes in sea surface level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 2
Physical features and ecosystem
The fjord landscape
/media/loftslag/Case_A___Horsens_Fjord.pdf