construction and maintenance.
7. Path dependency, meaning that roads will likely continue to exist even if the
underlying need for them decreases.
8. Social shifts, personal ownership of cars no longer seen as necessary. Car-sharing
becomes part of a suite of mobility options within the collective transportation
system.
9. Behavioral shifts, mobility no longer dominant variable in daily life
/media/loftslag/Group4.pdf
is completely saturated and the unsaturated zone no
longer active. The net horizontal boundary outflow is the
Figure 5. Observed and simulated groundwater heads at locations A and B in Figure 2.
W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE
9 of 18
W00A15
net outflow across the catchment boundary and accounts
primarily for groundwater flow to the sea. Drain flow
includes drainage from groundwater
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
-corrected SPOT 5
high-resolution geometric (HRG) images with 2.5 m
2.5 m spatial resolution, acquired in the autumn 2003
and (4) airborne polarimetric synthetic aperture radar
images observed simultaneously to the 1998 EMISAR
images and the EMISAR DEM viewed as a shaded
relief image (Magnu´sson et al. 2005b).
We estimate the average specific net mass balance (in
m yr1 w. eq.) as
bn r
DV
A1 N
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
of communication. However, it could be
9
improved e.g. by making it more simple and easy to grasp. The list of publications is
important, but at present the publications cannot be downloaded. A future improvement
would be to have a list of downloadable publications. A substantial improvement would be
executive summaries of publications adapted for stakeholders. Fact sheets could be an
important
/media/ces/ces-oslo2010_proceedings.pdf
................................................................................................................... 8
Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9
Lidar measurements of Norwegian glaciers – an overview
Neil Arnold* and Gareth Rees .............................................................................................. 10
Calculation of glacier velocity from repeat
/media/vatnafar/joklar/Reykholt-abstracts.pdf
(DGPS) equipment
in 2001. Continuous profiles, approximately 1 km apart,
were measured in the accumulation zone and a dense net-
work of point measurements were carried out in the abla-
tion zone. Digital Elevation Models (DEMs) of the surface
and bedrock were created from these data (Fig. 2; Björns-
son and Pálsson, 2004). The estimated errors are at most
1–5 m (bias less than 1 m) for the surface
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
lying areas in the City is illustrated for present climate in Figure 5. It is
expected that the future water level of the Horsens fiord will increase by 1 meter by the end of this
century.
Station 270045: Upstream Lake Nørrestrand
0
0.5
1
1.5
2
2.5
3
3.5
4
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
1
2
3
4
5
6
/media/loftslag/Horsens_case.pdf
as river discharge and
water levels. Notices on avalanches and sea-ice
are shown; short articles and news are presented.
Furthermore, web and data portals can be accessed
through the web, which is available in both Icelandic
and English. IMO uses the social networking website
Facebook for communication and feed-back. A new
web-application (App) provides access to forecasts
and warnings
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
increased net precipitation and increased rainfall intensity put pressure on the sewage
system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding
storms could be as high as 2,5 meters.
The challenges have been divided into two main themes: sea level change and rainfall.
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
increased net precipitation and increased rainfall intensity put pressure on the sewage
system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding
storms could be as high as 2,5 meters.
The challenges have been divided into two main themes: sea level change and rainfall.
NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop
/media/loftslag/Case_A___Horsens_Fjord.pdf