and access to a valuable collection
of photographs of the Skaftá cauldrons and jökulhlaups in Skaftá, Gunnar Sigurðs-
son for help with the measurements and Snorri Zóphóníasson for information about
jökulhlaups and hydrological measurements in Skaftá.
I want to thank Magnús Tumi Guðmundsson for valuable discussion about this
work and for data on the level of the overlying ice cover on the cauldrons.
vii
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
developed during the second scenario workshop (WS2) did not include any original GEO-4
text, except for Economy First. WS2 stories contained largely new material reecting the view of the subgroups. Additionally, the
title of each story was changed, indicating the increased ownership of the stakeholders. The nal scenarios were entitled: Economy
First (EcF), Policy Rules (PoR), Fortress Europe (FoE
/media/loftslag/Kok_et_al._TFSC_published_2011.pdf
The hydrological simulations were performed with the Wa-
tershed Simulation and Forecasting System (WSFS) developed
and operated in the Finnish Environment Institute (Vehviläinen
et al., 2005). The WSFS is used in Finland for operational hydrolog-
ical forecasting and flood warnings (www.environment.fi/water-
forecast/), regulation planning and research purposes
(Vehviläinen and Huttunen, 1997
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
i
s
c
h
a
r
g
e
m
3
/
s
Observed 1961-90
MetNo-HIRLAM-HadCM3 A1B 2021-50
DMI-HIRLAM-ECHAM5 A1B 2021-50
SMHI-RCA3-BMC A1B 2021-50
Observed and modeled runoff , Aiviekste
0.00
20.00
40.00
60.00
80.00
100.00
120.00
Observed Modeled Reference
mod SMHI
1961-90
mod SMHI
2021-50
Reference
mod DMI 1961-
90
mod DMI
2021-50
Reference
mod MetNO
1961-90
mod MetNO
2021-50
MAM JJA
SON DJF
m3/s
Monthly
/media/ces/Kurpniece_Liga_CES_2010.pdf
AN ENSEMBLE OF REGIONAL
CLIMATE CHANGE SCENARIOS FOR
THE NORDIC COUNTRIES
Erik Kjellström, Martin Drews, Jens
Hesselbjerg Christensen, Jan Erik Haugen,
Hilde Haakenstad and Igor Shkolnik
A changing climate in the Nordic region
Climate change in Northern Sweden:
Comparing 2071-2100 vs 1961-1990 (SRES A1B)
Lind & Kjellström, 2008
A changing wind climate in the Nordic
region?
DJF MAM JJA SON/media/ces/Kjellstrom_Erik_CES_2010.pdf
um íslenska jökla í árslok Overview of Icelandic glaciers at the end of
Upplýsingarnar sem hér birtast eru byggðar á mælingum jöklahóps Jarðvísindastofnunar Háskólans ( ), Veðurstofu Íslands (), Landsvirkjunar (), Náttúrustofu Suðausturlands (
) og Jöklarannsóknafélags Íslands (Jör). Nánari upp lýs ingar um sporða -mælingar veitir Bergur Einars son (bergur@
vedur.is), um afkomu
/media/Eplicanámskeið/VAT_newsletter_2018_06.pdf
The largest increase is simulated for the fall (SON, September-November),
when the average Vg increases by 2 to 4 % (Fig. 4). In the area of highest statistical significance, 9-10
models out of 10 agree on the sign of the change. Considering the months of December-February (Fig.
5) or the whole windy season September-April (Fig. 3), the increase is mostly 0 to 2 %.
Fig. 3. 10-GCM mean per cent
/media/ces/CES_D2.4_task2_CMIP3_winds.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
1
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1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574
POLICYFORUM
combined with opera-
tions
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf