and in a
brief written report at the end of the course. A break-out group is composed of 2-3 students.
Imagine that the group is part of a policy agency responsible for designing a long term (20 years) planning process that should enable the society to cope with
the climate change effects and its uncertainties allowing sufficiently robust and flexible management practices. We would then ask
/media/vedurstofan/NONAM-PhD_program.pdf
change
in Denmark is based on climate change projections for the period 2071–2100 for the IPCC
Mitig Adapt Strateg Glob Change
A2 and B2 SRES scenarios, using climate scenario data from the HIRHAM4 model
(Christensen et al. 1996), as utilized in the European climate downscaling project
PRUDENCE (Christensen et al. 2007a). According to these projections, Denmark will
probably warm by approximately 1
/media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
the uncertainty is great. For simplicity, the earthquakes are positioned with sea level as a referral plane.
Coloured patches on the surface represent the 20 most recent earthquakes. As the coloured patches move on they leave a gray color, which consequently shows where the activity has been. Doing is learning and our users are encouraged to test out the interactive possibilities:
zoom in and out
/earthquakes-and-volcanism/articles/nr/2971
the uncertainty is great. For simplicity, the earthquakes are positioned with sea level as a referral plane.
Coloured patches on the surface represent the 20 most recent earthquakes. As the coloured patches move on they leave a gray color, which consequently shows where the activity has been. Doing is learning and our users are encouraged to test out the interactive possibilities:
zoom in and out
/earthquakes-and-volcanism/articles/nr/2971/
:30 in the night before and saw a slide in the area where the large landslide was subsequently released, but this slide did not reach the river. Therefore, it seems that a small landslide was first released from the mountainside, and then the main slide occurred ca. five hours later. The debris is up to 20-30 m thickThe landslide fell from an area that showed evidence of earlier ground
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley
:30 in the night before and saw a slide in the area where the large landslide was subsequently released, but this slide did not reach the river. Therefore, it seems that a small landslide was first released from the mountainside, and then the main slide occurred ca. five hours later. The debris is up to 20-30 m thickThe landslide fell from an area that showed evidence of earlier ground
/about-imo/news/a-large-landslide-falls-in-hitardalur-valley/