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/about-imo/the-web/iframes/wind-temp-precip/
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/about-imo/the-web/iframes/wst-txt-obs/
in Reykjavík in 1909. The seismograph was a Mainka instrument and it was sent from Germany under the auspices of the International Seismological Association (ISA). The seismograph measured the horizontal north-south component of the ground motion and the records were sent to Strasbourg for analyzing. In 1913 another seismograph of the same type was installed in Reykjavík that measured east-west
/earthquakes-and-volcanism/conferences/jsr-2009/100_years/
active system in Iceland. The activity has changed in terms of frequency and type of eruptions with time. The period 9000-7000 years ago was dominated by effusive basaltic volcanism, the period 7000-3000 years ago was characterized by infrequent but large explosive silicic eruptions at the central volcano, and the last 3000 years have been dominated by more frequent and smaller mixed silicic
/volcanoes/about-volcanoes/hekla/hekla-eruptions/
:
Type of the magma and its viscosityThe steepness of the slope surface.If the magma flows as one big spread or in a
narrow channel or a magma tunnel.The rate of the magma coming from the ventBasaltic magma can flow tens of kilometers from the eruption
vent and the margin of the lava can go up to 10 km/hour depending on slope.
Usually the transport time is shorter, but if the slope gradient
/volcanoes/volcanic-hazards/lava-flow/
also includes multi-stakeholder processes
in planning and maintenance; however, as it is characterised by a relatively more
centralised (top-down) type of management.
2 NONAM stands for: Nordic Network for Adaptive Management in Climate Change Adaptation Planning. It is
funded by the Top Research Initiative of the Nordic Council of Ministers
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
process in which the effect of adopted water management measures must be monitored and
adjusted in an iterative way as new information and technology gradually become available
under changing and uncertain external impacts, such as climate change. This paper
identifies and characterises uncertainty as it occurs in the different stages of the IWRM
process with respect to sources, nature and type/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
Probabilistic daily streamflow forecasts
based on the combined use of a
hydrological model and an analogue
method
Philippe Crochet
VÍ 2014-006
Report
Probabilistic daily streamflow forecasts
based on the combined use of a
hydrological model and an analogue
method
VÍ 2014-006
ISSN 1670-8261
Report
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
150
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
the day and can be checked anytime. A personal weather watch will send notifications when certain criteria are met, e.g. a forecast of temperature below zero at your chosen weather station.
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/about-imo/news/nr/2812
away from the eruption site, but it can also accumulate around the site. Increased accumulation leads to the reservoir becoming unstable and the release of a jökulhlaup. Jökulhlaups from Eyjafjallajökull in 2010 are an example of this type of flood. In large eruptions, such as Katla eruptions underneath Mýrdalsjökull, ice melting can be very rapid and substantial in volume, resulting in large
/volcanoes/volcanic-hazards/glacial-outburst/