and to list categories of stakeholders such as water
users, potential groundwater pollution sources, and autho-
rities in the area including: local waterworks; water
consumers; farmers; industry; anglers; the local county;
and three municipalities. The stakeholder involvement
process and the extension of the organisation with new
Define context
Collect dat
a
Define states
Identify factors, ac
tion
s
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
flood hazard and flood risk mapping and flood risk management
planning by 2011–2015. The directive advises that the impacts of
climate change on the occurrence of floods should be taken into ac-
count when assessing the flood risks. It also poses new demands
for general evaluations of changes of flood discharges, flood inun-
dation areas and possible flood hazard due to climate change in dif
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
and CNES, n.d.;
National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional
altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein
et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea
level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013
/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
to highly
negative summer balances, but also lower bw than
the average for 1949–2006. Calculated change in
specific mass balance for a ±1°C change in air tem-
perature was ±0.55 m w.e., whereas a ±10 % in-
crease in precipitation represented a change of ±
0.20 m w.e. Model results further indicated that for
a 2°C warming, the ablation season will be extend-
ed by c. 30 days and that the period
/media/ces/GA_2009_91A_4_Andreassen.pdf
the maximum discharge of jökulhlaup water at the glacier
terminus is estimated as 97 m3 s 1. This jökulhlaup was a fast-rising jökulhlaup as
other jökulhlaups in Skaftá and cannot be described by the traditional Nye-theory of
jökulhlaups. The total volume of flood water was estimated as 53 Gl. The average
propagation speed of the subglacial jökulhlaup flood front was found to be in the range
0.2–0.4 m 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
for Iceland were made. The CE
project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different
emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate
Change (IPCC). The GCMs used by the CE project showed more warming during winter than
summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from
3–6 K, and from 2
/media/ces/2010_005_.pdf