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-
risk management - Part 2
Eriksson
Exercise work - how to
combine into a general
adaptive management
framework
PhD students
10:45 - 11:00 Coffee Coffee Coffee Coffee Coffee
11:00 - 12:45
Stakeholder involvement
methodologies - Part 1
Hare
Exercise work
PhD students
Scenario building
methodologies - Part 2
Kok
Uncertainty - concepts and
tools - Part 2
Refsgaard
Case in adaptive
management
/media/vedurstofan/NONAM-PhD_program.pdf
This is also the case with
cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected
by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are
cyclones in the neighbouring sector, in which case pressure tendencies are reversed.
21
Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com-
posite mean
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
support
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
of adaptive
management in relation to climate change
adaptation
• To introduce students to tools and methodologies in
topics of importance for adaptive management
– scenario development
– stakeholder involvement
– risk perception
– uncertainty assessments
– socio-economics
Multidisciplinary
Teachers
• Kasper Kok, Wageningen University, The
Netherlands
• Louise Eriksson, Umeå University
/media/loftslag/Refsgaard_1-Welcome.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
To distinguish between rain and snow, the volume is com-
pared to the water equivalent but the volume of snow is ten times larger.
Figure 1. How PWD22 determines the type of precipitation.
Using the information about the changes of the backscatter signal, water equivalent and temper-
ature the Vaisala Present Weather Detector can give information about the type of precipitation.
It is also used
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
development:
Experiences from the SCENES project
Kasper Kok a,, Mathijs van Vliet a, Ilona Bärlund c, Anna Dubel b, Jan Sendzimir b
a Wageningen University, P.O. Box 47, 6700 AA Wageningen, Netherlands
b International Institute for Applied Systems Analysis, Schlossplaz 1, A-2361 Laxenburg, Austria
c Helmholtz Centre for Environmental Research (UFZ), Brückstrasse 3a, 39114 Magdeburg, Germany
a r t i c
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf