conference
10.9.2010
The final conference of the CES project "Future Climate and Renewable Energy - Impacts, Risks and Adaptation" was held in Oslo from 31 May to 2 June. The conference was organised around five themes:
Past and present changes in climate
/about-imo/news/nr/1983
On October 31, a glacier outburst flood (jökulhlaup*) emerged from beneath the Skeiðarárjökull glacier, a southern outlet of the Vatnajökull ice cap. The floodwaters originate in the subglacial lake Grímsvötn, 50 km upstream from the glacier margin. The lake has been a source of such floods for centuries, but the size of the floods has varied greatly. The present flood is small and no threat to roads
/hydrology/articles/nr/2040
On October 31, a glacier outburst flood (jökulhlaup*) emerged from beneath the Skeiðarárjökull glacier, a southern outlet of the Vatnajökull ice cap. The floodwaters originate in the subglacial lake Grímsvötn, 50 km upstream from the glacier margin. The lake has been a source of such floods for centuries, but the size of the floods has varied greatly. The present flood is small and no threat to roads
/earthquakes-and-volcanism/articles/nr/2040
Thursday evening. Those who are interested in attending, are encouraged to apply for participation.The deadline for registration is 31 August. The abstract submission deadline is 15 September. The venue is Grand Hotel Reykjavík. Rooms have been reserved and can be booked through the registration process, although participants are of course free
to book other accommodation.Wide range
/about-imo/news/nordic-seismology-seminar-in-iceland
August 2022 showing new dike intrusion on Reykjanes Peninsula and deformation associated with the M5.47 earthquake on 31 July 2022. Coloured fringes show ground deformation in the satellite's line-of-sight, related to the new dike intrusion beneath Fagradalsfjall which commenced on the 30th July 2022. The interferogram shows approximately 16 cm of northwestward displacement related
/about-imo/news/status-of-unrest-in-reykjanes
earthquakes of M>=4 have occurred, and one 5.4 event at 17:48 on 31 July. A M4.0 earthquake has also occurred SV of Lake Kleifarvatn, at 08:02 1 Aug.
Cloud height:No eruption ongoing.
Other cloud information:No eruption ongoing.
Remarks:More information about this volcanic system is available at: https://icelandicvolcanos.is/?volcano=KRY
/earthquakes-and-volcanism/volcanoes/vona-notifications/
0.501.05 12:17:2553.56.8 km NW of Grímsfjall
0.601.05 11:38:13Check.6.9 km NNW of Grímsfjall
0.301.05 11:36:41Check.7.7 km NE of Krýsuvík
0.701.05 11:31:58Check.4.6 km SE of Bárðarbunga
0.501.05 10:53:07Check.5.1 km S of Fagradalsfjall
1.001.05 09:20:04Check.3.1 km E of Flatey
0.501.05 08:53:41Check.4.8 km W of Þrengsli
0.901.05 08:35:09Check.2.4 km NE
/m/earthquakes/latest
Sea ice was closest to land 31 nm NW of Barði, 25 nm NW of Straumnes, 19 nm NA of Horn and 43 nm NNW of Skagatá. Some floe and strip strayed off the main ice edge.
Another survey was done 13th December: The main ice was closest to land 53 nm WNW of Grímsey, 32 nm NNW of Skagatá, 32 nm ENE of Hornbjarg, 25 nm north of Hornbjarg, 20 nm WNW of Straumnes and 30 nm WNW of Barði.
Surveillance off
/sea-ice/monthly/2010/nr/2347
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Oslo, Norway, 31 May - 2 June 2010
At the Nordic and Baltic conference on “Future Climate and Renewable Energy ? Impacts, Risks and Adaptation”, you will meet stakeholders from the energy sector and researchers to exchange views and acquire information about current research results regarding the:
past and present changes in climate
/ces/events/nr/1739