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• 1. Volcanic plumes and tephra

  trajectory. The altitude that the plume can reach depends on several factors, primarily on the mass flux of the eruption. Other environmental factors, like wind field and atmospheric stratification, act on the plume dynamics affecting the final top altitude. Very strong wind can bend the rising mixture causing a lower top altitude and the maximum plume height to be located downwind the eruptive /volcanoes/volcanic-hazards/volcanic-emissions/

• 2. FAQ

  on the plume dynamics affecting the final top altitude. Very strong wind can bend the rising mixture causing a lower top altitude and the maximum plume height to be located downwind the eruptive vent. The type and style of the eruption also affect the plume altitude as well as the size of the erupted material. Pyroclastic material in the plume is subjected to two main forces: the force of gravity /volcanoes/grimsvotn-activity/faq/

• 3. Travel information

  or early afternoon leaving ample time to catch the workshop bus that departs from the main bus terminal in Reykavík at 18:00 on Wednesday 19 June arriving at Reykholt hótel, see map below, around 19:30. Those who want to rent their own car can check e.g. Avis or Europcar car rentals, or check their favourite car rental search engines. There will be a bus from Reykholt to Reykjavík on Friday /lidar/lidar-2013/travel-info/

• 4. Staff members

  Email: gs (hjá) vedur.is Division: Infrastructure Divsion Hydrological observation networks. Search Search /about-imo/employees/persona/126/fyrirtaeki/2

• 5. Weather stations

  EsjObs.ForecastMeteogramInfo.Obs. data Return to the top of the page Total number of stations: 290 Search Search string /weather/stations/

• 6. Sea ice in September 2011

  of Straumnes observed an iceberg 2-3 nm north of that location. Two observations were received from aircraft, on the 9th and 10th September. On the 13th, an observation was received from ship on icebergs in the following locations: 67°06.5N 026°43.5W 67°21.5N 026°21.8W 67°18.7N 026°12.2W 67°28.4N 026°40.5W 67°29.2N 026°53.4W 67°36.0N 026°35.7W 67°33.6N 025°49.9W Further observations /sea-ice/monthly/2011/nr/2405

• 7. News

  News null The location of the fracture at the top of Svínafellsheiði discovered in 2014. (Map from Daniel Ben /about-imo/news/bigimg/3671

• 8. News

  News null A GPS instrument sitting on the top of Mt. Þorbjörn. The town of Grindavík in the background. (Photo /about-imo/news/bigimg/3950

• 9. The weather in Iceland 2006

  at Kvísker in the Southeast on 20 December, 175.3 mm. Back to top The seasons and the individual months The winter (December 2005 to March 2006) was very warm, in Reykjavík and Akureyri it was the fourth warmest since the inception of continuous measurements. Overall the snowfall was very light, especially in the usually snowy areas of the North and East. In Reykjavík (the Southwest) the days /about-imo/news/2007

• 10. The weather in Iceland 2006

  at Kvísker in the Southeast on 20 December, 175.3 mm. Back to top The seasons and the individual months The winter (December 2005 to March 2006) was very warm, in Reykjavík and Akureyri it was the fourth warmest since the inception of continuous measurements. Overall the snowfall was very light, especially in the usually snowy areas of the North and East. In Reykjavík (the Southwest) the days /about-imo/news/2007/