-
work. The second half of the article discusses the potential for participatory modelling to progress from being a
mainly research-driven activity in the water sector to one being adopted for widespread use by water managers.
By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers
set up their own organizing teams, independent of researchers
/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
of the chapters can be downloaded or short summaries read.Downloadable material:Full text (pdf 23 Mb)Front matter (pdf 180 Kb)Table of contents (pdf 7.9 Kb)Chapter I. Volcanogenic floods in Iceland: An exploration of hazards and risks (pdf 1.06 Mb)Pages 7–16Emmanuel Pagneux, Sigrún Karlsdóttir, Magnús T. Gudmundsson, Matthew J. Roberts og Víðir ReynissonShort summaryChapter II. Öræfajökull Volcano
/volcanoes/about-volcanoes/oraefajokull/new-research/
in Eos.
How do I find weather forecasts for Iceland?
Information on the weather conditions near the volcano can be viewed on the weather pages of the IMO-web and navigated from there; for the areas near Eyjafjallajökull choose South or Southeast. The text forecast is most reliable but maps with specific wind-, temperature- and precipitation forecasts are automatic. There are no highland stations
/earthquakes-and-volcanism/articles/nr/1880
• Isostatic land rise, coastal changes, problems in
harbour management
Water on Earth as an average ocean depth
or sea-level rise equivalent
Am ount (m )
The world oceans 3500–4000
Antarct ica 56.6
Greenland Ice Sheet 7.3
Small ice caps and glaciers 0.2–0.4
Permafrost 0.03–0.1
Glaciers in Iceland 0.01
Glaciers and sea-level rise/GRACE
Velicogna, I., and J. Wahr. 2006. Measurements
/media/ces/Johannesson_Thomas_CES_2010.pdf
glacier inventories, aerial
photographs and expert judgement must be used to complete the curve down to the origin of the
figure. The volume distribution may then be computed by transforming the glacier area on the
y-axis of the area distribution curve in Figure 3 to volume using Equation (5) resulting in
V (vn) =
n
i=1
csgi ; (6)
in case the cumulative area distribution function V (v
/media/ces/ces-glacier-scaling-memo2009-01.pdf
M
(171FT
)
FRE
Q
UENCIE
S
(PE
R
CENT
)
O
F
OCCU
R
RENC
E
O
F
CONCURREN
T
WIN
D
DIRECTIO
N
(I
N
30
0
SEC
T
ORS
)
AN
D
SPEE
D
(I
N
KN
O
TS
)
WITHI
N
SPECIFIE
D
RANGE
S
ANN
U
A
L
WIN
D
WIN
D
SPEE
D
(KT)
)
DIRECTIO
N
CAL
M
1–
5
6–1
0
11–1
5
16–2
0
21–2
5
26–3
0
31–3
5
36–4
0
41–4
5
46–5
0
>5
0
T
O
T
A
L
V
ARIABL
E
0
0
0
0
0
0
0
0
0
0
0
0
0
35-36-0
1
3
2
3
3
2
1
1
0
0
0
0
0
14
02-03-0
4
0
2
4
4
3
1
0
0
/media/vedur/aerodrome_summaries_20140603.pdf
by parametric methods. Hydrology Research 39, 425-436.
Jónsdóttir, J. F., Uvo, C. B. (2009). Long-term variability in precipitation and streamflow in Iceland and relations to atmospheric circulation. Int. J. Climatol. 29, 425-436. doi: 10.2166/nh.2008.002.
Lawrence, D., Haddeland, I. Uncertainty in hydrological modelling of climate change impacts in four Norwegian catchments. Hydrology Research
/ces/publications/nr/1943
-010-0075-y.
Halldór Björnsson, Tómas Jóhannesson & Árni Snorrason (2011). Recent climate change, projected impacts and adaptation capacity in Iceland. Í: Linkov, I. & T. S. Bridges (ritstj.). Climate. Global change and local adaptation. Results of the NATO Advance Research Workshop, Hella, Iceland, 6.-10. júní 2010. NATO Science for Peace and Security Series - C: Environmental Security. Springer
/about-imo/arctic/completed-projects/publications/
Bárðarbunga GPS displacements
Subsidence Vertical displacement in the Bárðarbunga caldera
Gas observ. Volcanic gas detected
Gas observ. I want to report
Gas observ. View public observations
Gas observ. Handheld meters results
Gas observ. Hazard zoning
Gas forecast Text and maps approved by meteorologist on duty
Gas model Gas
/earthquakes-and-volcanism/articles/nr/2947