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  • 41. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 42. How do you view volcanoes?

    ? 28.2.2017 The Icelandic Met Office and King's College London are carrying out a survey on views toward volcanoes. It has two aims: to investigate Icelanders' and tourists' views about the 2014–15 eruptions at Holuhraun, and to assess the role of volcanoes /about-imo/news/how-do-you-view-volcanoes
  • 43. 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
  • 44. VI_2016_006_rs

    horizontal displacement of the most active part of Þófi since the start of the measurements is mostly in the range 10–35 cm (maximum 69 cm), whereas the movement in Neðri-Botnar is slower, with the more active points having total displacement mostly in the range 5–10 cm (maximum 46 cm). The maximum measured velocity of the horizontal movement in the Þófi area was 92 cm/a over a two-month period in late /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
  • 45. 2010_012rs

  • 46. Eyjafjallajokull_SK_20101214_1

    ash suspension was serious and a SIGMET was issued. Measurements and modelling development ongoing. IMO – London VAAC intercation IMO informes London VAAC every 3 hr, and more frequently if needed about: Plume height Plume activity (height and variation in height) Color/shade of the plume lightning activity seismic and hydrological activity surface and upper air observations (e.g. PIREP /media/vedurstofan/myndasafn/Eyjafjallajokull_SK_20101214_1.pdf
  • 47. A FUTUREVOLC exercise

    and running models to determine information such as the mass eruption rate. All of this was done in real time. To evaluate downstream dissemination of information, the exercise included the London Volcanic Ash Advisory Centre (VAAC) and representatives from the international media and civil protection. The recently released FutureVolc datahub and Catalogue of Icelandic Volcanoes were also tested /about-imo/news/nr/3277
  • 48. Web-pages related to the Grímsvötn eruption 2011

    This is an overview of web-sites related to the Grímsvötn eruption in 2011: Update on the volcanic eruption 21 - 30 May Photos from the eruption 21 - 25 May Vatnajökull monitoring (larger area) Lightning detection system from the UK Met Office (current lightning only) VAAC Volcanic ash advisory in London (current information only) Institute of Earth /earthquakes-and-volcanism/articles/nr/2220
  • 49. Ash cloud extending to Europe

    aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/nr/1873
  • 50. Ash plume and lightnings

    casts a dark shadow to the west: For flight traffic concern, please consult London VAAC, the Volcanic Ash Advisory Centre. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 /about-imo/news/nr/2177

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