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• 61. Safetravel

  measure of leaving a travel plan behind. Travel Plan One of the most important things to do when preparing a journey is to make a detailed travel plan and leave with someone who can act if needed. Travel plan should always include the following information: Date of travel, departure time and arrival time Names of those who travel and information on relative or contact Accommodation (GPS /about-imo/news/nr/2878

• 62. Safetravel in winter

  plan behind. Travel Plan One of the most important things to do when preparing a journey is to make a detailed travel plan and leave with someone who can act if needed. Travel plan should always include the following information: Date of travel, departure time and arrival time Names of those who travel and information on relative or contact Accommodation (GPS coordinates) and other places /about-imo/news/nr/3220

• 63. Climate and Modeling Scenarios

  : Impacts, risks and adaptation, Oslo, 31 May-2 June 2010. Ólafsson, H. & Rögnvaldsson, Ó. (2008). Regional and seasonal variability in precipitation scenarios for Iceland. In O. G. B. Sveinsson, S. M. Garðarsson & S. Gunnlaugsdóttir (Eds.), Northern hydrology and its global role: XXV Nordic hydrological conference, Nordic Association for Hydrology, Reykjavík, Iceland August 11-13, 2008, pp 623-629 /ces/publications/nr/1680

• 64. 2011_005

  contains a list of stations that have been off-line for at least two weeks in the spring of 2011. Table 3. Off-line stations. Station ID Station name Category Problem BALD Búrfellsalda við Kárahnjúka A Receiver is not logging. Needs to be reset ENTA Enta B No data from University of Iceland FITC Fitjarás B Data link down since 12-04-2011 HAUC Háumýrar B Poor radio link HVEL Hveravellir B /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 65. Bardarbunga_kafli20140825

  tephra (km3): Max: ~10 km3 Fallout beyond 1000 km: At least one in last 1100 years Tephra <63µm at 30 km ~5% Bulk volume lava (km3): Max: >20 km3 Longest lava flow: >130 km Gas emissions, sulphur: Significant to large depending on magma volume, max known 150 Mt SO2 Seismic characteristics Quiet between eruptions except for the region 10-15 km north of the caldera. No information on previous /media/jar/Bardarbunga_kafli20140825.pdf

• 66. VI_2015_005

  water. Since, in this study, the focus is on large-scale storm systems, persisting for at least one day, variability on shorter time-scales (mainly the diurnal cycle and atmospheric tides) is eliminated by calculating averages from the four 6-hourly reanalysis fields of each day (6-hourly precip- 8 Figure 1. Top: Average fields of 500 hPa geopotential height in winter (DJF 1989-90) and summer (JJA /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 67. GA_2009_91A_4_Andreassen

  and Geography 235 extended. Since then mass balance has been meas-ured at 6–10 stakes, snow depth at 100–150 pointsalong sounding profiles, and snow density at one ortwo locations (Fig. 1). The mass balance at Stor-breen is calculated using the stratigraphic method,i.e. between two successive ‘summer surfaces’(surface minima). Consequently, the measure-ments describe the state of the glacier after /media/ces/GA_2009_91A_4_Andreassen.pdf

• 68. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  of addressing the manifold biases that are present within decision-making. There are over 30 identified cognitive biases, on top of social biases, memory biases, belief biases, and so on. It would be impossible to create an analytic frame that can adequately encompass this many different variables. So one of the other dilemmas that I would like to explore with other researchers at the workshop is how /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 69. Water_resources_man_Veijalainen_etal

  is characterised by temperature-sensitive snow-dominated seasonality, with snow accumulating during N. Veijalainen (B) · T. Dubrovin · M. Marttunen · B. Vehviläinen Finnish Environment Institute, Helsinki, Finland e-mail: noora.veijalainen@ymparisto.fi Author's personal copy 3438 N. Veijalainen et al. winter and snowmelt during spring. This makes the area especially susceptible to major seasonal /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 70. Publications 2019

  weather stations and manual observations Ingibjörg Jóhannesdóttir51 1,0 2019-003 Hekla volcano monitoring project. Report to ICAO Sara Barsotti, Michelle M. Parks, Melissa A. Pfeffer, Matthew J. Roberts, Benedikt G. Ófeigsson, Gunnar B. Guðmundsson, Kristín Jónsdóttir, Kristín S. Vogfjörð, Ingvar Kristinsson, Bergur H. Bergsson, Ragnar H. Þrastarson57 4,9 /about-imo/publications/2019/