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
Of Precipitation In Latvia. XXV Nordic Hydrological conference, Northern Hydrology and its Global Role, 11-13 August, 2008, Reykjavik, Iceland. ISBN 978-9979-68-238-7. NHP Report No. 50, P. 134-142.
Hisdal, H., Barthelmie, R., Lindström, G., Kolcova, T., Kriauciuniené, J. & Reihan, A. (2007). Statistical Analysis. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role
/ces/publications/nr/1943
the A1B scenario. In the panels for
winter and autumn, contour interval is 25 MJ m−2, in those for spring and summer 50 MJ m−2. The
colour scale is the same in all panels.
Fig. A5. The absolute insolation change under the A2 scenario.
11
Fig. A6. The absolute insolation change under the B1 scenario.
12
(B) TIME SERIES
Fig. A7 shows the time series of seasonal changes in incident radiation
/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
the correlation between the
different predictors:
MD(u) =
q
(X(t) X(u))TS 1(X(t) X(u)) (5)
14
where X(t) (o1(t); ::;o j(t); :::;ok(t)) and X(u) (o1(u); ::;o j(u); :::;ok(u)) denote the multivariate
feature vectors at times t and u and S the covariance matrix.
The N best analogues correspond to those N days with the lowest ED or MD score. The ED
score has traditionally been used with nearest-neighbor
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
á við um aðrar veðurstöðvar innarlega í firðinum. Utar er úrkomuákefð norðanáttarinnar
meiri. Eyjafjörður stýrir vindi í stefnu sína. Í ríkjandi norðaustan- og norðanáttum er vindátt á
Akureyri því yfirleitt úr hánorðri eða af áttum vestan við norður. Langmestur hluti úrkomu á Ak-
ureyri fellur þegar vindur er á milli 290◦ (um norður) yfir í 20◦ og ákefðin er mest þegar vindur
blæs úr 330◦.
Mikil
/media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
(). The circulation of Icelandic waters-a
modelling study. Ocean Science , –.
Nygaard, B. E. K., Hálfdán Ágústsson & K.
Somfalvi-Toth (). Modeling wet snow ac-
cretion on power lines: improvements to previ-
ous methods using years of observations.
Journal of Applied Meteorology and Climatology
(), –.
Philippe Crochet (). Sensitivity of Icelandic
river basins to recent
/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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