bodies of management,
decision-support, risk, and participation literature.
d’Aquino (2008)
Patrick d’Aquino relies on 20 years of
implementation and evaluation experience, mostly
in a natural resource management context and in
developing countries. His approach is, at this point,
the least conceptually developed design method of
the guides presented here, although it is linked to a
theoretical
/media/loftslag/vonKorff_etal-2010.pdf
approximately centred around Iceland: the outer domain with
43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 9590 grid
points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The
northwest corner of the outer domain covers a part of the southeast coastal region of Greenland.
Otherwise, the only landmass included in the model domain
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
-1996
– 1997-2002
– Post 2002
Overall Effect of Wind Speed on
Damages
Damaged Homes By Wind Categories
100
120
0
20
40
60
80
< 120 120-
129
130-
139
140-
149
> 149
P
e
r
c
e
n
t
Damaged Homes (Cum.
Percent)
Average Home Size By Year
Built Categories
Average Home Size By Year Built Categories
2450
2500
2550
2150
2200
2250
2300
2350
2400
Pre 1980 80-96 97-2002 Post 2002
Avg. Sq. Feet
Damaged Homes
/media/loftslag/FMI_-_Disaster_Mitigation.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
12 1 month 12
Columbia River Basin Water Resource Sensitivity
to PCM Climate Change Scenarios
0%
20%
40%
60%
80%
100%
120%
Portland-
Vancouver
Spring Flood
Control
Reliability
Portland-
Vancouver
Winter Flood
Control
Reliability
Autumn Firm
Power
Reliability
(November)
% of Control
Hydropower
Revenues
McNary
Instream
Target
Reliability
(April-
August)
Middle Snake
Agricultural
/media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
Reykjavík, 139 pp.
Paterson, W.S.B. 1994. The Physics of
Glaciers (Third Edition). Pergamon. 480
pp.
Vogt, P.R., G.L. Johnson and L. Kristjánsson
1980. Morphology and magnetic anomalies
north of Iceland. J. of Geophysics 47, 67-80.
Walker, G.P.L. 1974. Eruptive mechanisms in
Iceland. In L. Kristjánsson, ed. Geodynamics
of Iceland and the North Atlantic Area. D.
Reidel, Dordrecht
/media/jar/Jokull-guidlines.pdf
conditions as a lower
boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic
run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run
must be considered as spin-up time for the ocean module. The RCAO run is experimental
since the model is in a development state and the output has not yet been evaluated over
Greenland (Ralf Döscher, personal
/media/ces/ces_geus_paakitsoq_full_report.pdf
of Time-
Variable Gravity Show Mass Loss in Antarctica. Science,
311, 5768, 1754 – 1756. DOI: 10.1126/science.1123785.
Wouters, B., D., Chambers and E. J. O. Schrama. 2008.
GRACE observes small-scale mass loss in Greenland.
Geophys. Res. Lett., 35, L20501, doi:10.1029/2008GL034816.
Meier, F. M., and others. 2007. Glaciers Dominate Eustatic
Sea-Level Rise in the 21st Century. Science, 317,
1064–1067
/media/ces/Johannesson_Thomas_CES_2010.pdf
Estimation of eruption site location
using volcanic lightning
Þórður Arason
Guðrún Nína Petersen
Halldór Björnsson
VÍ 2013-006
Report
Estimation of eruption site location using
volcanic lightning
V Í 201 3 - 006
ISS N 167 0 - 8 261
Report?
+354 522 60 00
ved u r@ ve d u r. is
Veð u rst of a Ísla n d s
Búst a ð a ve gur 7–9
150 Reykja vík
Þórður Arason, Icelandic Met
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf