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and direction, as well as air temperature, from the IMO operational surface station net-
work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some
stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m.
3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary
data file: grib_set -f -d 0.0 -w
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000/
in the data used in making the
decision and the factors are interlinked, all of which makes
the problem highly complex. The part of the net defined by
variables and links is relatively easily communicated to
stakeholders (Henriksen et al., 2007b). However the
tal Management 88 (2008) 1025–1036
quantitative part, with the conditional probability tables
(CPTs), the numbers, is the step where
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
-SAR's office leads the project with the help of many SAR team members as well as others with thorough experience in travelling in Iceland in different conditions. Safetravel is supported by a number of sponsoring companies.
112 Iceland app
An option is 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave
/about-imo/news/nr/2878
night and day, all year round.
112 Iceland app
Safetravel provides 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave their "trail" in case of search. From Safetravel's web-site, the app can be downloaded for either Android phones, Windows phones or iPhone:
First of all you can call for help by pressing
/about-imo/news/nr/3220
that, the detrended timeseries would have had a net difference of
zero if the negative values had not been set back to zero. This shows that over the 39 years of
data, there was a slight precipitation increase for this grid-point. This trend has been removed,
resulting in a detrended, almost flat dataset.
29
Figure 14. Regression lines for hourly precipitation timeseries of grid-point [100, 100]
from
/media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
grundvelli myndatöku með
flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu
flóðfara og við mat á útbreiðslu og umfangi hlaupa.
Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða
grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta
undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og
myndun gosrása staðfest af meiri nákvæmni en áður. Þó
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p.
Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562.
Linnerud, Kristin (2009) Climate change
/ces/publications/nr/1941