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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
............................................................................................................... 33
Lidar measurements of the cryosphere
Reykholt, Iceland, June 20–21, 2013
3
CryoSat-2 Arctic sea-ice freeboard and thickness data product and its validation
Ciaran Robb, Ian Willis and Neil Arnold ............................................................................ 34
Using airborne remote
/media/vatnafar/joklar/Reykholt-abstracts.pdf
E-mail: nve@nve.no
Internet: www.nve.no
May 2010
2
Contents
Snorrason, Á. and Hisdal, H.
Welcome to the conference “Future Climate and Renewable Energy: Impacts, Risks and Adaptation” ................ 6
PRESENTATIONS
Gode, J. and Thörn, P.
Stakeholder relevance of the CES project
/media/ces/ces-oslo2010_proceedings.pdf
), it was decided to broaden the remit to include both mitigation and adaptation
measures across the broad range of transport systems.
Expected main climate effects for Finland in relation to the national road network: 1)
Wetter winters with lower snowfall and more rain, 2) increase in freeze/thaw cycles in
winter in the southern parts of Finland, 3) higher frequency and severity of storms, 4)
hotter
/media/loftslag/Group4.pdf
to the annual temperatures
during 20032007. The low AAR and the high mass
balance sensitivity (e.g., Jo´hannesson 1997) to a uni-
form temperature rise (Table 4) at both Torfajo¨kull and
Tindfjallajo¨kull during the warm last decade are con-
sistent with their low and narrow elevation range
(Fig. 1).
Table 3 (a) Average specific net balance (bn), at the Eyjafjallajo¨kull (E), Torfajo¨kull
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
near the middle of the 21st century
and ∼2–3 ◦C by the end of the century, relative to the 2000–
2009 average. When compared to the reference period 1981–
2000, when the net balance of most of the Icelandic ice caps
was close to zero (Guðmundsson et al., 2011; Aðalgeirsdót-
tir et al., 2006; Guðmundsson et al., 2009b), the temperature
increase is 2.0–2.4 ◦C near the middle of the 21st century
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
, Veðurstofu Íslands
Contents
1 Introduction ................................................................................................ 7
2 Model setup and data ................................................................................... 7
3 Model terrain and surface type ...................................................................... 9
4 Impact of initial conditions in blending
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
networks for
t
i Christiansen Barlebo
r Voldgade 10, DK-1350 Copenhagen K, Denmark
form 3 May 2007; accepted 11 May 2007
29 June 2007
www.elsevier.com/locate/jenvman
Mak
manage
ARTICLE IN PRESS
brought together to find a solution that is adequate from
multiple perspectives. This, not only requires coping with
various sources and types of uncertainty, but also with the
ambiguity produced
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
in MIKE SHE / MIKE 11 in order to
describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3)
Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure
also show major highways, main roads and the topography in the area.
NONAM Summerschool Copenhagen 22-26 August 2011 3
Figure 3 Zoom in on Horsens by area. Hansted å
/media/loftslag/Horsens_case.pdf