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Flugleið:
Flugskýrsla TF-SIF
30. nóvember 2010
Flug nr. 16910.025
Texti:
Kl.0941, skipaumferð á NA- og A- landi.
Kl.0948, kallað í Havfrakt OZ2056 á ch-16. Hann er að koma frá Þórshöfn í Færeyjum og er á
leið til Þórshafnar á Langanesi
/media/hafis/skyrslur_lhg/16910025.pdf
three dimensional video - NEW
20.8.2014
The Bárðarbunga seismic activity can be explored in three dimensional videos which show the earthquakes.
16 - 26 August 2014
In this video, earthquakes near Bárðarbunga are shown in time and in three dimensions over a period
/earthquakes-and-volcanism/articles/nr/2948
Consultation meeting
Nordic Meteorological Institutes
3.9.2013
The Director General of the Icelandic Meteorological Office invited his colleagues of the other Nordic Meteorological Institutes to the northern town of Ísafjörður 26 – 28 August
/about-imo/news/nr/2736
in the afternoon. Decreasing wind and precipitation tomorrow evening and night, least though in Vestfirðir, the West fjords.
24 February 2015 at16:26
Meteorologists on duty
Teitur Arason and Haraldur Eiríksson
News
2023
2022
2021
2020
2019
/about-imo/news/nr/3090
A FUTUREVOLC exercise
12.2.2016
Over three days at the end of January 2016 all 26 FutureVolc partners, together with additional Stakeholders, were involved in responding to an evolving eruption scenario. The exercise was a great test of the new instrumentation
/about-imo/news/nr/3277
shows the current position of the station (m a.s.l.).
The graph (enlarge) was published 26 Sept. Now it shows the subsidence from 28 Sept until 4 Oct 2015. The total lowering of the ice-surface is shown by the value above the photograph (Heildarsig).
The red line shows the median value of relative displacement for every 30 minutes. This presentation was possible throughout the event because
/hydrology/research/skafta-cauldron/
Stóra Laxá. The combination of mild weather and intense rain is also encouraging snow to melt, which further contributes to the ongoing flood.
At 13:00 today, 26 February, the discharge of Hvítá at Fremstaver, in the northern part of the catchment, was 520 cubic metres per second. It will take floodwater in this region several hours to drain south, so maximum discharge will not be reached
/about-imo/news/nr/2660
15.0W
9) 67 05.0N 21 52.0W
10) 66 57.0N 22 32.0W
11) 67 00.0N 23 00.0W
12) 66 38.0N 25 00.0W
13) 66 30.0N 26 40.0W
Næst landi var ísinn á eftirfarandi stöðum:
1. 48 sjml vnv af Grímsey.
2. 46 sjml ana af Horni.
3. 34 sjml norður af Skagatá.
4. 25 sjml nnv af Sraumnesi.
Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að
sigla í gegnum
/media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
Eruption in Eyjafjallajökull
Status Report: 17:00 GMT, 26 May 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University
of Iceland
Compiled by: Hjörleifur Sveinbjörnsson, Teitur Arason and Sigrún Hreinsdóttir
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data;
web cameras, ATDnet – UK Met. Offices lightning detection system, Satellite
/media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf