drought-supporting
WTs over previous n days (n = 1, 15, 30, 45, 60, 90, 120, ... 330).
Determination of the period of influence: dreg
90
45 little groundwater45
45
CES conference, Oslo, Norway, 31 May - 2 June 2010
210
60
45
60
highly productive
aquifers
moderately
productive
aquifers}90
210
60
60
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe
/media/ces/AnneFleig_May2010_CES.pdf
will be compared to possible problems to
see if this is actually a problem. The completeness of the data series is discussed in section
6.
Table 7. Power connection.
Type of communication Number of stations
Main Power 35 (55%)
Produced on site 28 (45%)
For CGPS stations reliant on remote power sources, the preferred solution is a photovoltaic
solar panel and a wind generator. However, several
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
-
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
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf
in
estimation of climate change impacts on flooding. Generalisations based on only a few case studies, or
large scale flood assessments using only a few climate scenarios should be avoided in countries with var-
iable hydrological conditions.
2010 Elsevier B.V. All rights reserved.
1. Introduction
Climate change has a multifaceted impact on river discharges:
on the one hand it poses a risk of increased
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf