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11. Terms and conditions

but the information obtained is not personally identifiable. The Icelandic Meteorological Office is not responsible for any harm or damage that may result from incorrect or missing data on its web-site. By using the IMO web-site you agree to the terms and conditions stated on this page. Anyone can download images (photos) as they appear on our web-site (low resolution) but IMO does /about-imo/the-web/conditions/

12. The final CES conference, 31 May-2 June 2010

to exchange views and acquire information about current research of climate changes and energy issues. Altogether 31 oral presentations and 21 posters were presented at the conference, including 5 keynote presentations given by invited speakers from leading research institutes on climate and energy issues. The extended abstract volume of the presentations in PDF-form is available for download /ces/nr/1979

13. VI_2021_008

times because two distinct types of tremor were seen preceding the eruption. Volcano Name and Date of Summit Eruption Stat. Visual tremor arrival ALERT tremor detection Summit Eruption Time Max Warning Time 2.0-4.0 Hz 1.0-2.0 Hz 0.5-1.0 Hz 2.0-4.0 Hz 1.0-2.0 Hz 0.5-1.0 Hz Grímsvötn Dec. 28, 1998 skr 03:35, 09:12 03:36, 09:01 03:35, 08:58 03:40, 08:21 03:40 /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

14. VI2010-006_web

). Með því er átt við að áhættan sé svo lítil að ekki sé ástæða til að grípa til neinna aðgerða til þess að auka öryggi. Staðaráhætta sem svarar til þessa gildis getur verið mismunandi vegna breytilegrar gerðar og styrks bygginga og mismunandi dvalartíma fólks í þeim. Að öðru jöfnu er reiknað með að fólk dvelji allt að 75% af tíma sínum á heimilum og allt að 40% í atvinnu- húsnæði. Samkvæmt /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

15. VI_2016_006_rs

................................................................................. 38 Open channels....................................................................................... 38 Channels filled with gravel ....................................................................... 40 7.3 Protection measures for the settlement below Botnabrún................................. 41 Drainage ditches in Neðri-Botnar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

16. Mid-Latitudes-Agenda1_nov2013EH

Agenda *All presentations will be in the Forgardur (forecourt) underground basement room of the IMO building at Bustadavegur 7, unless otherwise noted. Wednesday, 13 November Time Agenda Item 09:00 – 09:15 Welcome and Introductions - T Jónsson and E Hanna 09:15 – 09:30 Meeting Structure and Overview - J Overland and E Hanna 09:30 – 10:40 09:30 – 09:45 09:45 – 10:05 10:05 – 10:25 /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

17. Kriauciuniene_Jurate_CES_2010

of temperature anomaly (ºC) between 1991-2007 and 1961-1990 Variation of annual T anomaly (ºC) between 1991-2007 and 1961-1990 Seasonal differences of P anomaly (in %) between 1991-2007 and 1961-1990 Seasonal differences of Q anomaly (in %) between 1991-2007 and 1961-1990 Variation of annual P and Q anomaly (%) between 1991-2007 and 1961-1990 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

18. Sitemap

19. Session program Thursday 13. October

on the long- and on the short-term before large earthquakes Ragnar Stefánsson 10:10 – 10:40 Coffeebreak and poster session 10:40 – 12:10 Oral session - Chair: Peter H. Voss 10:40 – 11:00 High-rate GPS seismology in Iceland Halldór Geirsson et al. 11:00 – 11:20 Rock stress boundaries deduced from rock stress measurements /norsem/norsem2016/program/thursday

20. News

News © Snorri Zóphóníasson Bridge across Ölfusá at Selfoss 26 February 2013 at 16:40. Flood due to rain and snow /about-imo/news/bigimg/2662

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