scenario
development, with an example from Brazil
Kasper Kok *
Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands
1. Introduction
The world is undergoing rapid changes while globalising
constantly, which gives the consideration of the future new
urgency and importance. Scenario development has emerged as a
key method when taking
/media/loftslag/Kok_JGEC658_2009.pdf
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a comprehensive assessment of the impact of climate change on
renewable energy resources in the Nordic area including hydropower, wind power, bio‐fuels and
solar energy.
M i bj i f h CES P j
An increase of uncertainty about the future of renewable resources under climate change is a key issue for the
energy sector. Some renewable energy resources are likely to increase their productivity
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/media/loftslag/Group-1_Scenarios-for-AWM.pdf
performance of the
model.
REFERENCES
Førland, E. J., Allerup P., Dahlström B., Elomaa E., Jónsson T., Madsen H.,
Perälä J., Rissanen P., Vedin H. and Vejen F. 1996. Manual for operational cor-
rection of Nordic precipitation data. DNMI Report No. 24/96 Klima, 66 pp.
Benoit, R., Pellerin P., Kouwen N., Ritchie H., Donaldson N., Joe P. and Soulis
E. D. 2000. Toward the use of coupled atmospheric
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
site, larger than yesterday.
White (steam) plumes rising from Gígjökull outlet glacier, north of the
eruption site smaller than yesterday.
Tephra fallout: According to the police at Hvolsvöllur there was ash-fall in Álftaver
and Meðalland, 65-80 km east-south-east of Eyjafjallajökull, where
people could hardly see next farms (in a few kilometres distance).
Lightning: No detections today
/media/jar/Eyjaf_status_2010-05-04_IES_IMO.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
................ 91
Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F,
Brennisteinsfjöll-Bláfjöll. ................................................................................. 92
Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93
Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active
between January
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
). Presentation and review of some methods for regional flood frequency anal-
ysis. J. Hydrol., 186, 63–84.
GREHYS. (1996b). Inter-comparison of regional flood frequency procedures for Canadian rivers.
J. Hydrol., 186, 85–103.
Grover, P.L., Burn, D.H. & Cunderlik, J.M. (2002). A comparison of index flood estimation
procedures for ungauged catchments. Can. J. Civ. Eng., 29, 731–741.
31
Hoskings, J.R.M. & Wallis
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf