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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

  between M4,0-5,0. The strongest one was M4,9 last night, 5. December, at 21:53. About 50 earthquakes were detected in the dyke of the same period, most of them smaller then M1,0. One earthquake was M2,0 yesterday, 5. January, at 02:26.  Seven earthquakes were detected in Tungnafellsjokull glacier during the period. The strongest one was around M3,0 on 30. December at 16:51.  GPS /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

  5 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 60 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 Appendix: Description of the usage of the ACER method to find return periods and an adopted Hunter method to calculate allowances in Norway . . . . . . . . . . . . . . 73 1 Introduction The dynamic /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 50. Bardarbunga_Daily_status_report_290814

  Heading No plume now, but winds were about 10 m/s from SE during the night. Colour No plume now. Tephra fallout No tephra fall now. Lightning No lightning during eruption according to ATDnet of the UK Met Office and WWLLN-system. Noise None. Meltwater The eruption was 5 km N of the glacier, therefore without a jökulhlaup. No indication of changes in water flow in rivers. The conductivity still /media/jar/Bardarbunga_Daily_status_report_290814.pdf