Sabbaticals
Information
Campaign
MM 1, 5, 10 Year
Guidance Plans
Check against EU
level (regulations
and directives)
2030 2040
Transport
Comissions Under
same umbrella
Regime Policy
(budget allocation,
goal setting,
authorization)
MM 1, 5, 10 Year
Guidance Plans
MM 1, 5, 10 Year
Guidance Plans
MM 1, 5, 10 Year
Guidance Plans
MM 1, 5, 10 Year
Guidance Plans
EVALUATION CYCLES / REFLECTION
1
/media/loftslag/Group4-Pres.pdf
PhD presentation of own
projects - 5 minutes per
student
Exercise work - plenary. End
of separate topics
Poster session +
refreshment
Course evaluation
19:00 - Course dinner
Lecturers and instructors Lectures Instructors - case study
Kasper Kok, Wageningen University Scenario building Part time
Matt Hare, Seecon Stakeholder involvement Part time
Louise Eriksson, Umeå University Acceptability
/media/vedurstofan/NONAM-PhD_program.pdf
82/2008, article 23) to change the scope of the access
controlled area north of Vatnajökull glacier. The decision is taken in close collaboration with the Icelandic
Meteorological Office, Vatnajökull National Park, the Icelandic Environmental Agency and the Directorate of Health.
At the end of January The Icelandic Meteorological Office carried out a new hazard assessment for gas pollution from
/media/jar/Access_conrolled_area_20150213.pdf
economic evaluation methods, the increasing drainage
capacity option can clearly be recommended. However, using other objectives the other
options may turn out favourably.
Mitig Adapt Strateg Glob Change
5 Discussion of climate change adaptation strategies under uncertainty
Our analyses of uncertainties, risks and adaptation characteristics have revealed a number of
key messages that are discussed
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
the operating system does not support the requirements or the hardware causes problems. But most of the users of en.vedur.is should be able to find their way to enjoy this product. A demo version is available below.
Instructions
The topography is exaggerated by factor 5, while depth in the model is not exaggerated. The depth of the earthquakes is indicated by two planes, at 5 km and 10 km, but in fact
/earthquakes-and-volcanism/articles/nr/2971
the operating system does not support the requirements or the hardware causes problems. But most of the users of en.vedur.is should be able to find their way to enjoy this product. A demo version is available below.
Instructions
The topography is exaggerated by factor 5, while depth in the model is not exaggerated. The depth of the earthquakes is indicated by two planes, at 5 km and 10 km, but in fact
/earthquakes-and-volcanism/articles/nr/2971/
displacements
and might be an old landslide deposit. The displaced material is a mixture of
e.g. rock debris, scree from the lower part of the hillside, swamp soil and
sediments from ancient lakes on the valley bottom. A preliminary estimate of
the volume of the slide is 10–20 million m3. The area
of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley
displacements
and might be an old landslide deposit. The displaced material is a mixture of
e.g. rock debris, scree from the lower part of the hillside, swamp soil and
sediments from ancient lakes on the valley bottom. A preliminary estimate of
the volume of the slide is 10–20 million m3. The area
of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley/