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  • 21. VI_2013_006

    stability, e.g. CAPE, in global numerical weather prediction models to mask out potential thunderstorm areas. Such a global system might be useful to monitor large areas of poorly monitored volcanoes, e.g. the chain of volcanoes in the Aleutian Islands, with its heavy air-traffic above. Conclusions An automatic monitoring system has been developed that estimates eruption site location based /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
  • 22. Kok_JGEC658_2009

    and that paving major roads will lead to deforestation. C3: Conservation units. A large percentage of the Amazon (close to 33%) is classified as some kind of protected area. This includes indigenous reserves, federal parks and national parks. Only about 5% is strictly protected, although it is argued that ‘paper parks’ can also be effective. C4: Forest accessibility. The amount of forest /media/loftslag/Kok_JGEC658_2009.pdf
  • 23. An eruption in South Iceland

    Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas dispersion model /earthquakes-and-volcanism/articles/nr/1852
  • 24. Re-evaluation needed of the size of the hazard area

    field for about 300 meters distance and started a brush fire which can be seen on one of the two RÚV webcams. It is not clear what is causing these changes in volcanic activity, but changes in magma flow, the chemical composition of magma/gas, or possibly changes in the volcanic conduit cannot be ruled out. Considering these changes in activity, the size of the hazard area at the eruption site /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir
  • 25. A glimpse into the field

    because of the narrowing of the riverbed, caused by the lava. According to observations, that edge of the lava which has entered the river has not advanced this afternoon. Baugur alone Baugur in action and Suðri cool in the foreground. Photo: Ármann Höskuldsson. Crater Suðri had already ceased erupting when we approached the site. Only the central part of the fissure is now active /about-imo/news/nr/2985
  • 26. A glimpse into the field

    because of the narrowing of the riverbed, caused by the lava. According to observations, that edge of the lava which has entered the river has not advanced this afternoon. Baugur alone Baugur in action and Suðri cool in the foreground. Photo: Ármann Höskuldsson. Crater Suðri had already ceased erupting when we approached the site. Only the central part of the fissure is now active /about-imo/news/nr/2985/
  • 27. IPPC-2007-ar4_syr

    Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 28. Bárðarbunga 2014 - September events

    at 07:58 this morning in the nortern part of Bárðarbunga, M4.9, and it was accompanied by ca. 25 cm lowering of the caldera according to the newly installed GPS meter there. In the afternoon, two earthquakes close to M3.5 occurred, both in Bárðarbunga. Other earthquakes have been smaller. According to scientists in the field the activity has diminished and the only crater which is active, is the one /earthquakes-and-volcanism/articles/nr/3001
  • 29. Bardarbunga-2014_September-events

    occurred in northern Bárðarbunga about two o‘clock AM, size M 5.0 and therefore somewhat smaller than the earthquake there yesterday afternoon. In all, 17 earthquakes have been detected in Bárðarbunga this night, the majority at the northern caldera rim, but fewer in the intrusive dike under Dyngjujökull, only 8. Eruptive activity could not be monitored on web cameras because of weather /media/jar/Bardarbunga-2014_September-events.pdf
  • 30. Bárðarbunga 2014 - September events

    at 07:58 this morning in the nortern part of Bárðarbunga, M4.9, and it was accompanied by ca. 25 cm lowering of the caldera according to the newly installed GPS meter there. In the afternoon, two earthquakes close to M3.5 occurred, both in Bárðarbunga. Other earthquakes have been smaller. According to scientists in the field the activity has diminished and the only crater which is active, is the one /earthquakes-and-volcanism/articles/nr/3001/

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