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Ensemble approach for probabilistic
hydrological projections
Catchment
/media/ces/Lawrence_Deborah_CES_2010.pdf
). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
Session rapporteur allocation
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wide and
1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of
the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and
landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of
the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
opportunity, it is essential for any new methods to be
able to account for future potential. The Risk
Assessment Framework also accounts for the
identification of opportunities, and subsequently also
th i id ti i th d i i kirepresen , or e ec s on ma ers or o er
stakeholders, the risk analysis results in a efficient
and compact way.
encourages e r cons era on n e ec s on‐ma ng
process.
Fig.2. Fourfold
/media/ces/ces_risk_flyer.pdf
inty in decision making linking pluriform uncertainty combining certified and tacit knowledge
Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos
Eivind Junker Jussi Ylhäisi Athanasios Votsis
Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs
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estimation. NVE Report No. 1 - 2009, ISBN 978-82-410-0680-7; 44 p.
Meilutyté-Barauskiene, D. (2009) Impact of Climate Change on Runoff of the Lithuanian Rivers, Summary of Doctoral Dissertation, Technological Science. Environmental Engineering (04T). Kaunas University of Technology, Lithuanian Energy Institute.
Roald, L.A., Hisdal, H. & Lawrence, D. (2009). Hydrologi og skred før, nå og i fremtiden. I
/ces/publications/nr/1938
versa
• Very large range within the simulations
• Larger number of observation stations in the study area leads to
• better compatibility between different observational data sets
• smaller bias in the model simulations
CES Conference, Oslo 31.5.-2.6.2010
References
• Haylock, M. R., Hofstra, N., Klein Tank, A. M. G., Klok, E. J., Jones, P.
D. and New, M. 2008. A European daily high-resolution
/media/ces/TietavainenHanna_CES_2010.pdf
on the
Shifts of climatic
zones from
cooler or wetter
to warmer or
drier
(a) 1971-2000 (b) 2010-39 A1B
observational data set
(0.25º grid) from Haylock
et al. (2008)
(b-d) Based on CMIP3
GCM runs for A1B
& the delta-change
method
(c) 2040-69 A1B (d) 2070-99 A1B
Jylhä et al. (2010)
Uncertainties in climate change schematically
Observed
climate
Future
climate Natural
/media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf
We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below:
A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208