power, bio-fuels and solar energy. The CE project benefited from the national projects and extends and integrated their work both on a regional scale and for cross-cutting subjects. The projected climate changes will influence both the energy requirements and the possibilities of energy production. Furthermore, extreme weather events could impact the planning, design and operation of the energy
/climatology/research/ce/introduction/
IMO's Involvement in WMO's Global Cryosphere Watch
25.1.2018
Three years ago, the World Meteorological
Organization (WMO) approved the implementation of the Global Cryosphere Watch
(GCW) as a cross-cutting mechanism to bring together
/about-imo/news/imo-s-involvement-in-wmo-s-global-cryosphere-watch
-512.
Alam, A., Kilpeläinen, A. & Kellomäki, S. (2008). Potential carbon stocks and energy production in boreal forest ecosystems under climate change responsive to varying management regimes. Submitted Biomass and Bio-energy.
Kärkkäinen, L., Matala, J., Härkönen, K., Kellomäki, S. & Nuuttinen, T. (2008). Potential recovery of industrial wood and energy wood raw material in different cutting/ces/publications/nr/1939
The project will be organized as a matrix structure with work groups, WG, on the renewable energy resources. Cross-cutting issues are also delegated to WG. These WG will be supported and served by a Steering group with one representative from each of the partners. An Information management group will be responsible for information dissemination, active stakeholder involvement and the public outreach
/ces/project/
biomass along
with timber to substitute fossil fuels and to mitigate climate change.
Main objectives of the Bio-Fuels Working Group
The project is organized as a matrix structure with working groups, WG, on the renewable energy
resources. Cross-cutting issues are also delegated to WG. These WG will be supported and served by
a Steering group with one representative from each of the partners
/media/ces/CES_BioFuels_Flyer_new.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
www.sciencemag.or
g
Downloaded from
1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574
POLICYFORUM
combined with opera-
tions
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
Eruption on the fissure swarm north of Gjáfjöll mountain range. Effusive for ice free part – see 1a and
1b for glaciated part. Moderate to large (example: 1862-1864 CE Tröllahraun).
3. Eruption on the fissure swarm beyond 50 km from central volcano (~1 event/1000 years):
a. Southwesternmost part (Veiðivötn part) of the fissure swarm: Large or very large eruptions. Fissures
10-70 km long, cutting/media/jar/Bardarbunga_kafli20140825.pdf