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• 31. IMO's Involvement in WMO's Global Cryosphere Watch

  intern Aldís Elfarsdóttir contributed to the evaluation of candidate stations and global participation in the CryoNet, glacier best practices, and the compilation of scientific literature on observations of permafrost, freshwater ice, and ice sheets. These tasks took place in collaboration with GCW Project Manager, Rodica Nitu, GCW Website and Outreach Team Lead, Jeff Key, CryoNet Team Chair /about-imo/news/imo-s-involvement-in-wmo-s-global-cryosphere-watch

• 32. New seismic stations installed around Öræfajökull

  in the crust at a few kilometers depth. The 48-hours seismicity is available on the IMO website and updated in real-time. Scientists from IMO met on the 17 of October with colleagues from the Institute of Earth Sciences of the University of Iceland and representatives of the Civil Protection Department of the National Police. The purpose of the meeting was to review all the available monitoring /about-imo/news/new-seismic-stations-installed-around-oraefajokull

• 33. Warning for Sunday and Monday

  more dependable as they draw closer to events. With new information forecasts will be updated on IMO's website. Please note, that if the models on the webpage and the text forecasts differ, the text forecasts are valid. After a rather mild and calm November there is now a shift in the weather patterns around Iceland, and forecasts indicate rather unrestful weather for the next week. IMO Friday 28 /about-imo/news/nr/3020

• 34. Re-evaluation needed of the size of the hazard area

  in the crater. (Photo: Icelandic Institute of Natural History).Power of the eruption can be estimated from satellite informationTo assess the power of the eruption, it is also possible to use information from satellites that detect heat radiated from the Earth's surface. Such measurements can be seen, for example, on the website of the MIROVA project (Middle InfraRed Observation of Volcanic Activity /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 35. Sea ice in May 2010

  An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average /sea-ice/monthly/2010/nr/2340

• 36. Sea ice in October 2010

  2010 Sea ice in October 2010 One observation was received from a ship on an iceberg 22nd October in location 67°39´N /sea-ice/monthly/2010/nr/2345

• 37. Minor jökulhlaup in Grímsvötn

  eruptions have occurred in Grímsvötn and the surrounding area in the last 200 years. The last eruption in Grímsvötn was in 2011 and it was quite large and powerful, but otherwise the last few eruptions have been rather small and lasted for a few days. More information about the volcano can be found at the Icelandic volcanoes website, https://icelandicvolcanoes.is /about-imo/news/minor-jokulhlaup-in-grimsvotn

• 38. HARMONIE - numerical weather prediction model 

  It is important to describe the surface, and its properties, as well as possible. To do this SURFEX uses elevation data (from the GTOPO3 database of USGS), data on sand- and clay fraction in soil (from the HWSD database of FAO) and data on land surface parameters (from the ECOCLIMAP-II). SURFEX Figure 1. The processes simulated with the model SURFEX (from the SURFEX website). The current set-up /weather/articles/nr/3232

• 39. Wind Energy

  Conference, Indianapolis, October 2007. 10 pp. Clausen, Niels-Erik (2008). Et bud på fremtidens vindkraft-med vægt på landbaseret vind. Vind-workshop om arealplanlægning på Örenäs Slott 26.-27. nov. 2008. Pryor S.C. (2009). Wind climates: Variability and change. AWEA Fall conference on wind resource estimation. Orlando, Florida, November 2009. Other, Dissertations, Website, Talks (no proceedings /ces/publications/nr/1944

• 40. Sea ice in March 2007

  was well within the median and closest to shore, about 50n.m. NW off Straumsnes and 60n.m. W off Barði. The ice-edge density was extensively 4/10 or less than 7-9/10 north off 67°20'N. A considerable diagenis was discovered in the southernmost part of the exploratory territory. No other dispatches were made during the month. Easterly and later northeasterly winds were common in the Greenland /sea-ice/monthly/2007/nr/2300