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• 41. Station forecasts, text forecasts or observations

  Station forecasts, text forecasts or observations Station forecasts, text forecasts or observations Instructions on how to embed iframes /about-imo/the-web/iframes/wst-txt-obs/

• 42. Session program Wednesday 12. October

  Wednesday 12. October Session program Wednesday 12. October Oral presentation are 20 minutes long, 15 minutes talk plus 5 minutes discussion /norsem/norsem2016/program/wednesday

• 43. Volcanic gas detected

  All observations gasskráning Browse through all observations A more thorough web-viewer of public observations is available for those interested in browsing through all observations and seeing how they change with time. The viewing can be limited to certain days or periods of time. Adjust the scale below the map by using two handles to mark the chosen period. A short-cut to this viewer /pollution-and-radiation/volcanic-gas/

• 44. Volcanic gas detected

  All observations gasskráning Browse through all observations A more thorough web-viewer of public observations is available for those interested in browsing through all observations and seeing how they change with time. The viewing can be limited to certain days or periods of time. Adjust the scale below the map by using two handles to mark the chosen period. A short-cut to this viewer /pollution-and-radiation/volcanic-gas

• 45. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.pdf

• 46. Factsheet_Bardarbunga_20150106

  Data collected in flight over the lava field on 30th of December show that the volume of the lava field in Holuhraun is about 1,15 cubic kilometre.  Seismic activity in Bardarbunga continues to be strong, but it has though somewhat decreased. Total number of earthquakes in Bardarbunga from the last meeting of the board, on the 30th of December, is just over 250. About 20 earthquakes were /media/jar/Factsheet_Bardarbunga_20150106.pdf

• 47. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  climate change may alter the supply chains in forest and food industries, or indirectly via transport and environmental policy. The different freight transport modes and the competitiveness will be influenced the most by the mitigation measures and by how equally these measures are allocated globally and especially on the EU-level [5]. Also with respect to adaptation to climate change /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 48. Eriksson_1-Risk-perception

  of the hazard are related to how risky the hazard is perceived to be (e.g., dread, unknown, and exposure, Fischhoff et al. 1978) 4. Cultural theory (Douglas, 1978; Douglas & Wildavsky, 1982)- worldviews are important for how we respond to risks: egalitarians, individualists, hierarchists, and fatalists (Sjöberg, 2000) 4 (1) Environmental risks • Uncertain and have strongly delayed consequences, occurring /media/loftslag/Eriksson_1-Risk-perception.pdf

• 49. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 50. Bardarbunga_Daily_status_report_290814

  Bárðarbunga update 29082014 2014-08-29 16:20 UTC Bárðarbunga update Compiled by Icelandic Met Office and University of Iceland Þórður Arason (Ed.) Based on Seismic, GPS, Hydrology, Radar, Webcam, PIREP, visual observations Eruption plume Height (a.s.l.) No plume was detected by radar (detection limit above 1 km) and webcam indicated low level gases and steam from lava fountains during the night /media/jar/Bardarbunga_Daily_status_report_290814.pdf