planning; 2) a state-of-the-art
literature review, examining European and American municipal and regional adaptation strategies, 3)
interviews (20-30) with municipal and regional planners and policy makers in Copenhagen and Portland; 4)
the use of a Multi-Criteria Decision Support (MCDS) software tool to help understand how different groups
rank and value competing planning goals within
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
estimation. NVE Report No. 1 - 2009, ISBN 978-82-410-0680-7; 44 p.
Meilutyté-Barauskiene, D. (2009) Impact of Climate Change on Runoff of the Lithuanian Rivers, Summary of Doctoral Dissertation, Technological Science. Environmental Engineering (04T). Kaunas University of Technology, Lithuanian Energy Institute.
Roald, L.A., Hisdal, H. & Lawrence, D. (2009). Hydrologi og skred før, nå og i fremtiden. I
/ces/publications/nr/1938
on the
Shifts of climatic
zones from
cooler or wetter
to warmer or
drier
(a) 1971-2000 (b) 2010-39 A1B
observational data set
(0.25º grid) from Haylock
et al. (2008)
(b-d) Based on CMIP3
GCM runs for A1B
& the delta-change
method
(c) 2040-69 A1B (d) 2070-99 A1B
Jylhä et al. (2010)
Uncertainties in climate change schematically
Observed
climate
Future
climate Natural
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
to the troposphere and can therefore be distributed
over a large area, even the whole globe. In those instances, ash and volcanic
aerosols can cause a temporary cooling effect by reflecting the incoming solar
radiation, i.e. the volcanic cloud can have an impact on the climate. As an
example, the eruption in Pinatubo in the Philippines occurred in 1991. In that
eruption about 20 million tons of sulfur
/volcanoes/volcanic-hazards/volcanic-emissions/
and Finland. The event was located approximately 59 km SE of Piteå and 80 km NE of
Skellefteå in Sweden, while the distance to the nearest Finnish city, Raahe, was 100 km. The
earthquake was widely felt in northern Sweden and Finland, the furthest reports come from some 250
km away, with intensities up to V. The main event was followed by 6 aftershocks within the first 8
hours, and two
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf