finished,
and possibly tested before implementation starts
(Bots 2007).
Following Bots (2007), we note that the word
“design” can denote an activity as well as a product.
In this article, design as a product is synonymous
with the participation plan (point y). This plan is
based on design as an activity, represented here by
the space between points x and y. What needs to
happen in this phase (x/media/loftslag/vonKorff_etal-2010.pdf
(Quante and Colijn, 2016). Work on risk analysis and adaptation is in different
stages in the countries of the world.
Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do
so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the
probability of such events can rise with climate change (Almannavarnir, 2011
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
ISBN 978-9979-68-238-7. NHP Report No. 50, P. 638-645.
Kriauciuniene J. & Kovalenkovienė M. (2008). Dependence of Lithuanian river runoff extremes on atchment area. XII Biennal International Conference. Hydrological extremes in small basins, 18-20 September, 2008, Cracow, Poland. ISBN-978-83-88424-38-0. P.183-186.
Kriauciuniene, J., Kovalenkovienë, M., and Meilutytë-Barauskienë D. (2007). Changes
/ces/publications/nr/1943
: central Iceland (65◦N, 20◦W); bottom-left: southern Denmark (55 ◦N, 10◦E); bottom-right:
south-eastern Finland (62.5◦N, 27.5◦E).
6
The robustness of the response increases as the climatic warming proceeds. This can be
seen from Fig. A8 in the appendix, where probability distributions are given for the period
2070-2099. For example, at that stage in eastern Finland the probability of insolation
/media/ces/CES_D2.4_solar_CMIP3.pdf
ANNUAL REPOR T 2014
2
I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4
?Veðurstofa Íslands 2015
Bústaðavegur 7–9, 108 Reykjavík, Iceland
The annual report was drafted by the IMO sta?.
Editor: Sigurlaug Gunnlaugsdóttir
Design and layout: Hvíta húsið
Printing: Oddi
ISSN 2251-5607
Cover photo: Gro Birkefeldt Møller Pedersen
I N D E X
4 Bárðarbunga
7 Rockslide
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
when local information alone (method 2) is
not sufficient.
In order to take into account seasonal effects, a moving window of +/– 45 days centered on the
target day was considered for the selection of analogues, so that in an archive made of Y years,
each target day was at most associated to Y x91 potential analogues. The window size was
arbitrarily defined and not optimized. A similar window
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
Gíslason, Árni Snorrason, Jórunn Harðardóttir,
Svava Björk Þorláksdóttir, Árný E. Sveinbjörns-
dóttir & R. A. Neely (). Efnasamsetning,
rennsli og aurburður straumvatna á Austur-
landi X: Gagnagrunnur Jarðvísindastofnunar
og Veðurstofunnar. Raunvísindastofnun
Háskólans RH--, s.
Eydís Salóme Eiríksdóttir, Svava Björk
Þorláksdóttir, Jórunn Harðardóttir & Sigurður
Reynir Gíslason
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
Clausen, N.-E., Pryor, S. C., Guo Larsén, X., Hyvönen, R., Venäläinen, A., Suvilampi, E., Kjellström, E., Barthelmie, R. (2009). Are we facing increasing extreme winds in the future? EWEC 2009 Marseille session DT2A, 19 March 2009.
Engen-Skaugen,T & Førland, E.J. (2010). Future change in return values and extreme precipitation at selected catchments in Norway, met.no Report 20/2010 (draft).
Engen
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