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• 21. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions/

• 22. The final CES conference, 31 May-2 June 2010

  to exchange views and acquire information about current research of climate changes and energy issues. Altogether 31 oral presentations and 21 posters were presented at the conference, including 5 keynote presentations given by invited speakers from leading research institutes on climate and energy issues. The extended abstract volume of the presentations in PDF-form is available for download /ces/nr/1979

• 23. Traffc-maintenance_expenditures

  229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 24. Kok_2-scenarios-lecture-2

  extreem events C6; qual nat. systems C7; policies C8; price of resources C9; other sectors C10; industry C11; inrastructure Crimea - Ukraine Manaus - Brazil From FCM to model input FCM – strong points • Easy to develop and apply. The approach is highly intuitive, it can quickly be explained and applied to any new situation. • High level of integration. A FCM can contain any type of information /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 25. 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

• 26. Kok_et_al._TFSC_published_2011

  ]. There is ample experience with backcasting, and consequently much has been said about the underlying principles (e.g. [20]), the methodological 838 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy framework (e.g. [8,30–32]), and practical applications (e.g. [33–35]). Also the combination between backcasting and other types of scenarios has been /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 27. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 28. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 29. VI_2021_008

  off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 30. 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