was deployed and together with the permanent NNSN stations in that area it contained 33+
stations within span 350 x 200 km. About 1250 earthquakes of M>0.0 was recorded during the project
period and new map of seismicity of that area was retrieved.
The main aim of the project is to reveal the stress field in that particular region and therefore
determination of stable
/media/norsem/norsem_michalek.pdf
– observed and simulated changes in global mean
temperature
• Pattern scaling approach
– changes in mean climate and variability assumed to be
proportional to the change in global mean temperature
Regression coefficients of winter mean
temperature: how much is climate on the average
simulated to change per 1°C of global warming?
XX
Helsinki (60ºN, 25ºE): On average, the mean winter temperature
/media/ces/RaisanenJouni_CES_2010.pdf
........................................................................................................................... 3
Summary ............................................................................................................................... 4
Summary of the break-out sessions on road infrastructure ................................................... 6
Summary of the break-out sessions on Horsens case
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km.
During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another
/about-imo/news/nr/2183
a probability of an
adverse event occurring and a measure of the
associated event. Larger consequence and larger
probability lead to a larger overall risk (e.g. Risk =
Probability x Damage)
Conclusions – Part 1
Terminology
• Be aware of ambiguities in terminology used by others –
and be specific defining the terminology you use
Concepts
• Uncertainty assessment should influence the entire
/media/loftslag/Refsgaard_2-uncertainty.pdf
with whom a slot is proposed to
be swapped.
In the closing session on Friday afternoon another two Workshop participants will be offered the
opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will
require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in
time (Friday morning at the latest) who will present
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
; from which
extensive data streams enter IMO and are utilized
for forecasts and research purposes.
Dissemination
The main dissemination of IMO is in the form of
forecasts and warnings; through radio, T V, direct di-
alog with stakeholders and through IMO‘s web-site
(vedur.is). Additionally, the web provides compre-
hensive real-time data on the weather, earthquakes
and deformation, as well
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
Íslands
Bústaðavegur 9
150 Reykjavík
Abstract
Fast-rising jökulhlaups from the geothermal subglacial lakes below the Skaftá caul-
drons in Vatnajökull emerge in the Skaftá river approximately every year with 45
jökulhlaups recorded since 1955.
The accumulated volume of flood water was used to estimate the average rate of
water accumulation in the subglacial lakes during the last decade as 6 Gl
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
Scales as mentioned in Cash et al. (2006)
space time juris. inst. man. netw. know. other
Van Apeldoorn et al. 2011 XXX
Mandemaker et al. 2011 XXXX
Van der Veen and Tagel 2011 XXX
De Blaeij et al. 2011 XXXX (spatial) beneficiaries,
ecosystem services
Turnhout and Boonman-Berson 2011 XX
Van Lieshout et al. 2011 XX agricultural
juris. = jurisdictional
inst. = institutional
man
/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf