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about 28% and losses from the polar ice sheets
contributing the remainder. From 1993 to 2003 the sum of these
climate contributions is consistent within uncertainties with the total
sea level rise that is directly observed. {WGI 4.6, 4.8, 5.5, SPM, Table
SPM.1}
Observed decreases in snow and ice extent are also consistent
with warming (Figure 1.1). Satellite data since 1978 show that an-
nual average
/media/loftslag/IPPC-2007-ar4_syr.pdf
mean surface air temperature anomalies ....................................... 28
14 Surface air temperature anomalies over Scandinavia ...................................... 29
15 Composite mean precipitation anomalies..................................................... 30
6
1 Introduction
Extratropical low-pressure systems, persisting for at least a few days, have long been recognised
as one
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
to be simple and therefore has important drawbacks.
Future improvements should be made in the light of applications within a larger toolbox of scenario
methods.
2008 Elsevier Ltd. All rights reserved.
* Tel.: +31 317 482422; fax: +31 317 419000.
E-mail address: kasper.kok@wur.nl.
Contents lists available at ScienceDirect
Global Environmental Change
journa l homepage: www.e lsev ier .com/ locate
/media/loftslag/Kok_JGEC658_2009.pdf
level, surveys commissioned by the European Com-
munity/the European Union provide an indication of trends in concern about cli-
mate change. Since 1992, such surveys have been undertaken among representative
samples of citizens in its Member States, and specifically on topics related to the
environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB
in 2002). These have included
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
. . . . . . . . . . . . . . . . . 28
9 Weibull shape parameter at 50 and 100 mAGL for all wind directions . . . . . . . 30
10 Average wind power density based on corrected WRF model data . . . . . . . . . 33
11 Average wind power density based on NORA10 data . . . . . . . . . . . . . . . . 34
12 Differences in wind power density between northerly and southerly winds . . . . . 35
13 Directional
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
Simulation results
Hydropower
Thermal production
Energy balance
CO2-emissions
4 Summary and concluding remarks
Sintef Energy Research Quantitative system analysis 8 of 21
Introduction
Electricity system model
Simulation results
Summary and concluding remarks
Hydropower
Thermal production
Energy balance
CO2-emissions
Annual average in ow over the year, GWh
0 14 28 42 52
0
500
1;000
1;500
2;000
2;500
/media/ces/Mo_Birger_CES_2010.pdf
at the operational/local level.
A calibrated approach (standardized questionnaires and
interviews, expert judgment, and reinterpretation of out-
comes by means of relevant literature) was used to com-
pare the state of affairs in water management in the
selected case-studies.
Adaptive and integrated water management
Given the expected increase of climate-related extreme
events, water governance capabilities
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
km south-southwest of the
eruption site at 15:00 GMT.
Lightning: Four lightning strikes detected over the summit of Eyjafjallajökull between
19:47 and 20:03 GMT on 28 April.
Noises: Booming sounds were reported yesterday evening, and again this morning,
from Selsund, located ~40 km north-northwest of the eruption site.
Additional note: 16:13 GMT: A sulphur smell was detected at 3
/media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf