(See black box in the figure above. Click here for a larger view ). This fault was identified during the 2017 earthquake swarm
which also occurred in this area. The current earthquake activity is interpreted to be part of a
larger scale volcano-tectonic reactivation event in the Reykjanes peninsula. Localised subsidence signal
detected at SvartsengiThe satellite images also reveal a localised
/about-imo/news/update-on-the-activity-in-the-reykjanes-peninsula
........................................................................................................................... 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
:
m/s:
km/h:
knots:
Beaufort-values corresponds to windspeed intervals. If a number is entered in the Beaufort-box, other boxes will display appropriate median values for that Beaufort-number, approximated to the nearest integer. If a number is entered in other boxes, the Beaufort-box will display the approximated Beaufort-value. This approximation inevitable leads
/weather/articles/nr/1283
:
m/s:
km/h:
knots:
Beaufort-values corresponds to windspeed intervals. If a number is entered in the Beaufort-box, other boxes will display appropriate median values for that Beaufort-number, approximated to the nearest integer. If a number is entered in other boxes, the Beaufort-box will display the approximated Beaufort-value. This approximation inevitable leads
/weather/articles/nr/1283/
a systematic com-
parison of results to observed precipitation has been carried out. Un-
dercatchment of solid precipitation is dealt with by looking only at
days when precipitation is presumably liquid or by considering the
occurrence and non-occurrence of precipitation. Away from non-
resolved orography, the long term means (months, years) of observed
and simulated precipitation are often
/media/ces/Paper-Olafur-Rognvaldsson_92.pdf
- nitrate reduction in underground medium medium large large large
Model technical uncertainty
- numerical approximation small small medium small
- bugs in software medium medium small
SUM:
Importance Type of uncertainty
Error propagation
Box 1 Error propagation rules using standard deviation (σ )
Addition and Subtraction: z = x + y + .. or z = x - y - ..
..)()( 22 ++= yxz σσσ
/media/loftslag/Refsgaard_2-uncertainty.pdf
or click directly on a day or time.
The forecast of auroral activity at midnight, scale 0 to 9, is shown in the upper-right box. The scale changes in accordance with the date selected under the cloud cover map.
The timing of sunset, darkness, sunrise and moonrise are valid for Reykjavík.
Aurora activity, sun and moon -
Aurora forecast
/weather/forecasts/aurora/
on a day or time.
The upper-right box shows the forecast of auroral activity at midnight on the scale 0 to 9. The scale changes in accordance with the date selected under the cloud cover map.
Aurora forecast shows expected activity at your selected date. Even grade 2 (low activity) can be beautiful and grade 3 (moderate) can be dazzling.
The timing of sunset, darkness, sunrise and moonrise
/weather/articles/nr/2588
to
issue warnings and forecasts.
These data provide a benchmark for assessing ongo-
ing changes in the Arctic, valuable information on
natural resources in Iceland such as water and wind
resources, as well as being fundamental in risk as-
sessment studies carried out at IMO.
In order to broaden the research already carried
out at IMO the institute is involved in many multi-
participant
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf