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• 41. vonKorff_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Von Korff, Y., P. d'Aquino, K. A. Daniell, and R. Bijlsma. 2010. Designing participation processes for water management and beyond. Ecology and Society 15(3): 1. [online] URL: http://www. ecologyandsociety.org/vol15/iss3/art1/ Synthesis, part of a Special Feature on Implementing Participatory Water /media/loftslag/vonKorff_etal-2010.pdf

• 42. Bárðarbunga 2015 - March, April, May

  uplift of the caldera center were detected). 11 April 2015 - tourists' interest Iceland eruption trips are popular, according to the online version of Iceland Review, yesterday. However, precautions must be taken against the possibly hazardous fumes, see their earlier news: "Now that tourists can visit the Holuhraun eruption site, they must pay close attention to the levels of toxic volcanic gases /earthquakes-and-volcanism/articles/nr/3122

• 43. Bárðarbunga 2015 - March, April, May

  uplift of the caldera center were detected). 11 April 2015 - tourists' interest Iceland eruption trips are popular, according to the online version of Iceland Review, yesterday. However, precautions must be taken against the possibly hazardous fumes, see their earlier news: "Now that tourists can visit the Holuhraun eruption site, they must pay close attention to the levels of toxic volcanic gases /earthquakes-and-volcanism/articles/nr/3122/

• 44. Bardarbunga-2015_MarchAprMay-events

  that could be interpreted as water accumulation under the ice, could be seen (neither uplift of cauldron floors nor significant uplift of the caldera center were detected). 11 April 2015 - tourists' interest Iceland eruption trips are popular, according to the online version of Iceland Review, yesterday. However, precautions must be taken against the possibly hazardous fumes, see /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 45. Terms and conditions

  Meteorological Office's web-site: Unless stated otherwise, you are free to use data on this web-site; however, if the data are used for presentation or publication, reference must be made to the Icelandic Meteorological Office. The same stipulation applies to the graphical representation of IMO data. Unless stated otherwise, there are no restrictions on the use of IMO data, neither for private nor /about-imo/the-web/conditions

• 46. Terms and conditions

  Meteorological Office's web-site: Unless stated otherwise, you are free to use data on this web-site; however, if the data are used for presentation or publication, reference must be made to the Icelandic Meteorological Office. The same stipulation applies to the graphical representation of IMO data. Unless stated otherwise, there are no restrictions on the use of IMO data, neither for private nor /about-imo/the-web/conditions/

• 47. Protective measures

  resolution pdf for printing, 28 Mb; order free paper copies) Background for the determination of dam height in the SATSIE dam design guidelines (IMO Int. Rep. 08003, 2008, authors T. Jóhannesson, Kristín M. Hákonardóttir, C. B. Harbitz and U. Domaas) (pdf 1.0 Mb) Software for the computation of run-up of snow avalanches on catching and deflecting dams as well as on natural terrain /avalanches/imo/protective/

• 48. Workshop on Jökulhlaup Hazards

  17:30 Reception The workshop will be held at the Icelandic Meteorological Office (IMO), with attendance limited to ~20 participants due to the size of the venue. Attendance is free-of-charge and lunch will be provided; any access or dietary needs should be communicated via e-mail (see below). How to Attend If you wish to participate in the workshop, then please contact Matthew J. Roberts /about-imo/news/nr/2251

• 49. Bardarbunga_kafli20140825

  have extensive ice cover. The 2009 m high Bárðarbunga central volcano lies at the NW edge of the ice cap, with only its NW slopes ice free. It is dominated by a 80 km2 and up to 700 m deep ice-filled caldera. Bedrock rises to 1850 m in the northwest caldera rim and is lowest in a narrow gap the east rim where minimum elevation is 1350 m. The ice free fissure swarm north of Vatnajökull strikes /media/jar/Bardarbunga_kafli20140825.pdf

• 50. Journal_of_Hydrology_Veijalainen_etal

  -dimensional hydraulic model, Two-dimensional Unsteady FLOW (TUFLOW). It uses full two-dimensional, depth averaged, momentum and conti- nuity equations for free-surface flow calculations and an alternat- ing direction implicit (ADI) finite difference method as the computational procedure (TUFLOW, 2007). The geometry data of the river channel and flood plain for the 2D hydraulic model were from /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf