(2006). The impacts of climate change on the Nord Pool electricity market. Presented at the European Conference on Impacts of Climate Change on Renewable Energy Sources, Reykjavik, Iceland, June 5-9. [Extended abstract]
Hydropower, snow and ice:
Aðalgeirsdóttir, G. (2003). Flow dynamics of the Vatnajökull ice cap, Iceland: VAW/ETH Zürich, Mitteilungen no. 181.
Aðalgeirsdóttir, G. (2004
/climatology/research/ce/publications/
of ice melt at the
AWS location will increase from c. 40 to c. 80 days.
Key words: glacier, mass balance, albedo, temperature, precipita-tion, precipitation, climate
IntroductionTo predict how a glacier will react to climate
change or to reconstruct a glacier’s mass balanceback in time, a mass balance model is needed to
relate the surface mass balance to prevailing cli-
mate conditions. A whole
/media/ces/GA_2009_91A_4_Andreassen.pdf
permit subject to the Water Act to change
the outflow and thus avoid or reduce damages. Exemption permits have been used
since 1980 on average once in three years for several weeks at a time.
In Lake Pielinen an ongoing study examines the possibilities to change the
regulation of the lake. Currently the lake is regulated only in flood or drought
situations, but more intense regulation scheme has been
/media/ces/Water_resources_man_Veijalainen_etal.pdf
which, in Iceland, is defined to
begin on 1 September. Each one-year simulation is set up with a cold-start forecast ({BUILD-
yes}) on 31 August at 18 UTC, with a lead time of 6 hours ({LL-06}),
The initial conditions provided by ECMWF operational analyses introduce an unrealistically
high late-summer snow cover into the HARMONIE simulations. To avoid this, as well as asso-
ciated effects
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
at Bárðarbunga in mid August.
At the time of writing, there is a clear view of the eruption site from the Míla camera on Vaðalda. The last 24 hours of images show no obvious changes in the size or intensity of the eruption.
29 November 2014 - how the subsidence is monitored
Until recently, point measurements of the subsidence of the Bárðarbunga caldera were available in near real time as the IMO
/earthquakes-and-volcanism/articles/nr/3023
changes in earthquake rate have been observed several times since the unrest began at
Bárðarbunga in mid August.
At the time of writing, there is a clear view of the eruption site from the Míla camera on
Vaðalda. The last 24 hours of images show no obvious changes in the size or intensity of the
eruption.
29 November 2014 - how the subsidence is monitored
Until recently, point measurements
/media/jar/Bardarbunga-2014_November-events.pdf
at Bárðarbunga in mid August.
At the time of writing, there is a clear view of the eruption site from the Míla camera on Vaðalda. The last 24 hours of images show no obvious changes in the size or intensity of the eruption.
29 November 2014 - how the subsidence is monitored
Until recently, point measurements of the subsidence of the Bárðarbunga caldera were available in near real time as the IMO
/earthquakes-and-volcanism/articles/nr/3023/
their characteristics and describe how to deal with the different sources of uncertainties
o How are you representing and explaining uncertain knowledge to stakeholders?
3. Prepare a stakeholder involvement plan
o How do you achieve a common understanding among stakeholders?
o What are the overall objectives and principles of the stakeholder involvement?
Overall objective: Support decision making
/media/loftslag/Group5-Milestones.pdf