maps for 1971-2000
Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson.
Reference:
Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model
/weather/articles/nr/1625
Projections
-50%
-48%-73%
-78%
-80%
+3%
Storglaciären Mårmaglaciären
Scandinavia
Comparison with all other glacier regions
Volume reduction and sea-level equivalent (SLE)
until 2100 for 19 glacier regions
Radic and Hock, submitted
Antarctica
Sub-Antarctic Islands
Greenland
New Zealand
South America II
South America I
Iceland
Arctic Canada
West Canada and West US
Alaska
High Mountain Asia
North
/media/ces/Hock_Regine_CES_2010rs.pdf
Neotectonics in Nordland; NEONOR 2
C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf,
M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners
The Nordland shore region is known to be seismically active with deep local sediment basins on the
continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland
have
/media/norsem/norsem_lindholm.pdf
tímabilið 1949–2009.
T P1d P2d P3d P5d
1 22 29 35 43
2 26 35 41 51
5 32 43 50 61
10 36 49 56 68
20 40 55 62 75
50 46 62 71 85
og 5 daga tímabil fyrir veðurstöðina á Akureyri. Taflan sýnir úrkomu sem svarar til 1, 2, 5, 10,
20 og 50 ára endurkomutíma, þ.e. tölfræðileg greining bendir til að úrkoma verði ekki meiri en
sem nemur gildunum í töflunni oftar en endurkomutíminn segir til um þegar til langs
/media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
ll
l
ll l l
l l
l
l l
l
l l
l
H1−ROI: 0.848
H1−ROI+vhm167: 1.69
Figure I.3. As Fig. I.I but for vhm238 (top-left), vhm144 (top-right), vhm145 (bottom-left),
vhm167 (bottom-right).
28
Appendix II - Index flood estimation at gauged sites treated
as ungauged.
l
l
l
l
l
l
l
l l
l
ll
0 400 800 1200
0
50
0
100
0
150
0
Pred. (m³/s)
R
ef
. (m
³/s
)
µ(D)=(θ0)(A)(θ1)
Rel. RMSE= 0.87
NS= 0.8
MAE= 83
l
l
l
l
l
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
+ x−k) (1)
Public Choice (2012) 151:91–119 95
with k = 1,2, and −k = 1 if k = 2, −k = 2 if k = 1. The variables xik and x−k are the
contributions to the public good of subject i as mover k and mover −k, respectively. The
contribution of the first mover is an integer x1 ∈ [0,10] and that of the second mover takes
one of the two values x2 ∈ {0, x1}.
2.2 Theoretical predictions
As noted
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
to improve our world," says Esri president Jack Dangermond. "Each year I look forward to being part of this ceremony. It is a tradition that means a great deal to Esri and to GIS professionals."
More information is available about the 2011 Special Achievement in GIS Award winners, including project information and photos. There, examples of IMO's work can be seen
/about-imo/news/nr/2241
and sustainable society. The main vision of the European Plate
Observing System (EPOS) is to address the three basic challenges in Earth Sciences: (i) unravelling the
Earth's deformational processes which are part of the Earth system evolution in time, (ii) understanding
the geo-hazards and their implications to society, and (iii) contributing to the safe and sustainable use
of geo-resources
/media/norsem/norsem_atakan_ip.pdf
(2011) Horsens Fjord Case. Background document for case study, 18 pp.
Refsgaard JC, Henriksen HJ (2011) Horsens case - Break out groups. Tasks for group work. 3 pp.
Lorenzoni I, Pidgeon NF (2006). Public views on climate change: European and USA perspectives. Climatic Change, 77, 73-95. DOI: 10.1007/s10584-006-9072-z
Stern PC (2000). Toward a coherent theory of environmentally significant behavior
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
about 20-25% in 2010 to about 50% in 2050. Perhaps surprisingly,
a particularly high probability is found in Iceland, most likely as a result of the small
12
interannual variability there. As expected, the probability of very warn years rises even faster
than that of warm months – in northern Europe from typically 30-40% in 2010 to about 60-
80% in 2030 and to 85-95% or even more in 2050
/media/ces/CES_D2.4_task1.pdf