......................... 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
). NeWater is based on the
hypothesis that IWRM cannot be realised unless current
management regimes undergo a transition towards more
0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved.
doi:10.1016/j.jenvman.2007.05.009
Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50.
E-mail address: hjh@geus.dk (H.J. Henriksen).
(Downing et al., 2005). Vulnerability
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
) Finland the spring flood peaks are
currently by far the largest floods and as they mostly decreased
with climate change the magnitude of the annual 2 and 100-year
floods decreased. In the north (Fig. 8a) some scenarios still pro-
duced large spring floods in 2070–2099. In southern Finland (in
the coastal rivers Fig. 8e and in the lake area Fig. 8d) large floods
occurred not only in spring but also
/media/ces/Journal_of_Hydrology_Veijalainen_etal.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
farvegarins undir jöklinum út frá rúmmáli vatns
sem þar hefur safnast fyrir benda til þess að viðnám gegn vatnsrennsli við jökul-
botn minnki eftir því sem líður á hlaupið. Undir lok hlaupsins runnu á bilinu 80–
90 m3 s 1 um farveg sem var einungis einn þriðji hluti af rúmmáli farvegar sem flutti
svipað vatnsmagn á fyrsta eða öðrum degi eftir að hlaupið hófst við jökuljaðar. Þessi
niðurstaða er
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
developmen
t &
im
plemen
tat
ion
Inf
orma
tion
Ma
nagemen
t
Fin
an
ce
an
d Cost
Re
cover
y
Risk
Ma
nagemen
t
Eff
ec
tiven
ess
Inte
rna
t. R
egula
tion
Weighted averag
e
Rivierenland Alentejo Tisza Ukraine Tisza Hungary
Fig. 3 Level of Adaptive and
Integrated Water Management
in coping with climate-related
extreme events in the four case-
studies (0 = non-adaptive and
non-integrated, 2
/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