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• 51. VI_2009_012

  Mw(v) plotted against log distance. The coefficient of correlation between Mw(v) and log distance is 0.24. High correlation coefficients have been shown to affect parameter estimates in one step regression methods (see Fukushima and Tanaka, 1990). The Ci values were also calculated from the derived PGA values. Instead of constructing another magnitude scale based on acceleration it was decided /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 52. VI_2014_006

  to reduce systematic biases in the flow forecasts, if any, a recursive error correction procedure which builds on the algorithm proposed by Boi (2004) is defined, assuming that dis- charge observations are available in real-time and are of good quality. The algorithm establishes a correction to be applied on predicted discharge issued at time t0, based on the error between observed and analyzed /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 53. NONAM_1st_workshop_summary_v3

  ; in particular Chapter 4). 7 Seppo Saarelainen & Lasse Makkonen: Adaptation to climate change in the road management – Pre-study. Helsinki 2007. 8 The Finnish Road Administration (Finnra) (2009), The effect of climate change on the routine and periodic maintenance of roads, Finnra report 8/2009, (in Finnish, abstract in English). 9 Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 54. Ash carried southward and east

  is about 16,000 feet, periodically up to 24,000 feet. Winds from the north carry the ash southward, where westely winds in the upper atmosphere carry it towards the east. The wind directions are not expected to change much during the next few days. Check London VAAC for further information. Click on the link "Issued graphics" above the map, and choose the most recent map. Glacial floods /about-imo/news/nr/1879

• 55. 47th Nordic Seismology Seminar

  and then click on "Registration" on top of that page (see screenshot). Conference costs are 30.000 ISK (~220€), to be paid upon registration. See details on cancellation policies on the registration page. Rooms at Grand Hotel Reykjavík can be booked during the registration process. Participants are free to book other potentially cheaper hotels in the vicinity.Conference costs include coffee /norsem/norsem2016/registration/

• 56. PhD summer school

  Center for International Climate and Environmental Research - Oslo (CICERO), Norway Finnish Environment Institute (SYKE), Finland Government Institute for Economic Research (VATT), Finland Aalto University School of Science and Technology /nonam/events/nr/1928

• 57. VI_2020_011_en

  particles formed as the magmatic gases age (most notably, SO4 aerosol is formed from SO2 gas), and from tephra particles (the finest ash can be breathed in, and the acidic coatings on tephra particles can acidify and pollute fresh water). One person died due to CO2 accumulation in a basement during the 1973 Eldfell eruption. During the eruption, rescue 22 workers needed to be aware of escape /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 58. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 59. Notes on the 2010 eruptions

  the crater, supported by lower plume (2-4 km) according to radar. MODIS satellite image shows both ash from the volcanic site and loose ash blown from the surface of Mýrdalsjökull ice cap. Comments on sound blasts, viscosity, deflation and tremors. Link to satellite image RADARSAT-2 (from the Canadian Space Agency), link to a briefing issued by WMO of frequently asked questions. 25.04.2010 – 28.05.2010 /earthquakes-and-volcanism/articles/nr/2467

• 60. Significant ground

  commenced in December 2019. The unrest is ongoing and the occurrence of additional future earthquakes is considered likely. Click here for a larger image. Here is also a useful link on how to interpret an interferogram from our colleagues at USGS. News 2023 2022 /about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake