......................... 17
8 Monthly averages of SURFEX or projected 2-m air temperature ...................... 18
9 Local correction factors for 10-m wind speed ............................................... 19
10 Interpolated correction factors for 10-m wind speed ...................................... 20
11 Monthly averages of original or corrected temperature and wind speed .............. 21
12
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
Journal of Environmental Management 88
Heid
, Øste
d
e
A broad range of tools are available for integrated water resource management (IWRM). In the EU research project NeWater, a
Human dependence on water leaves us vulnerable to
climate change, flood and drought hazards, and poverty
dynamic element of vulnerable groups and their relation-
ship to water resources, and to represent the decisions
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
20
0
60
0
J F M A M J J A S O N D
0
20
0
60
0
J F M A M J J A S O N D
0
50
10
0
15
0
J F M A M J J A S O N D
0
50
10
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J F M A M J J A S O N D
0
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0
20
0
30
0
J F M A M J J A S O N D
0
10
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20
0
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J F M A M J J A S O N D
0
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0
120
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/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
(Quante and Colijn, 2016). Work on risk analysis and adaptation is in different
stages in the countries of the world.
Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do
so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the
probability of such events can rise with climate change (Almannavarnir, 2011
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
Av. Ed.
Belin, 31400 Toulouse, France
Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011
Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011
Abstract. The Little Ice Age maximum extent of glaciers in
Iceland was reached about 1890 AD and most glaciers in the
country have retreated during the 20th century. A model for
the surface mass balance
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
(alb: AWS)
MODELLING LONG-TERM SUMMER AND WINTER BALANCES
? The authors 2009
Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241
ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature
/media/ces/GA_2009_91A_4_Andreassen.pdf
was therefore formed
by ice lifting and deformation induced by subglacial water pressures higher than ice
overburden pressure.
The discharge data and the derived size of the subglacial flood path, as indicated
by the volume of water stored subglacially, indicates a development towards more
efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the
iii
range 80–90 m3 s 1
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
on the European level [e.g.
Water Framework Directive (Directive 2000/60/EC),
Common Agricultural Policy, etcetera], except for the
Ukrainian part of the Tisza. However, the Ukraine shows
strong incentives to enter the EU community and thus the
EU acquis communautaire is used as key reference for the
development of its water management principles. It was
nevertheless decided to select two case-studies
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
respec-
tively. Due to limited data availability, for the SMHI-RCAO run, the 20th Century control period
is restricted to the 20-year period 1971–90, and the second 21st Century reference period is limited
to the years of 2070–80. For the MetNo-HIRHAM runs, no data are available during the second
21st Century reference period.
3 Spatial Variability of Climate Trends
This section discusses
/media/ces/2010_005_.pdf