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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
with whom a slot is proposed to
be swapped.
In the closing session on Friday afternoon another two Workshop participants will be offered the
opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will
require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in
time (Friday morning at the latest) who will present
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
this
perspective, states do things differently nowadays
because they operate in different network
formations and use other instruments. However, in
this perspective the state is still the engine that keeps
the motor running. In contrast, society-centered
perspectives even consider the possibility of
‘governance without government’ (Rhodes 1996).
A particular type of governance concept that has
been thriving
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
for the cases where abstractions and
irrigation are not included (Table 3, top) and included
(Table 3, bottom). The results are spatially averaged, mean
annual values for the 15-year period. The net recharge is
defined as the outflow from the root zone minus the sum of
evapotranspiration and net flow from the groundwater zone
to the overland compartment for the grids where the soil
profile
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
21
15%
55
26
5%
5546% of world's GDP
2233% of world’s population
10%0%Runoff decreases by
Continental U.S. and Alaska
All scenarios Top 200 basins
Precipitation change per degree T change vs
evaporation change per degree T
All scenarios Top 200 basins
Precipitation change per degree T change vs runoff
change per degree T
A1B scenario Top 200 basins
Precipitation change per Degree T change
/media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
series, of which about 28,000 are from European
studies. White areas do not contain sufficient observational climate data to estimate a temperature trend. The 2 x 2 boxes show the total number of data
series with significant changes (top row) and the percentage of those consistent with warming (bottom row) for (i) continental regions: North America (NAM),
Latin America (LA), Europe (EUR), Africa
/media/loftslag/IPPC-2007-ar4_syr.pdf
Projects
involving sh
Concise info
Executive
summaries
Downloadable
"Stakeholder
friendly" info
Stakeholder Relevance of the CES Project
Jenny Gode, 31 May 2010
Research programme
"Translators"
F
act
sheets
W
eb
page
Stee
ring
co
m
m
ittee
Visits
W
o
rkshops
R
efe
re
nce
g
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up
s
E
x
.
su
m
m
a
rie
s
M
eetings
Stakeholders
Energy companies
Energy authorities
Decision makers
Other stakeholders
/media/ces/Gode_Jenny_CES_2010.pdf
of melt water from glaciated
areas in long integrations for a warming climate.
Glacier dynamics
This problem can be qualitatively analysed by considering the continuity equation for ice vol-
ume, which may be expressed as
¶h
¶t
+
¶q
¶x
= b or
¶h
¶t
+~ ~q = b ; (1)
for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions,
respectively. h is ice thickness, q or ~q
/media/ces/ces-glacier-scaling-memo2009-01.pdf