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  • 1. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971
  • 2. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971/
  • 3. 47th Nordic Seismology Seminar

    buy a "Flybus Plus" ticket, further transportation from BSÍ terminal in central Reykjavík to the hotel is included. Get a return ticket for smooth transportation back to the airport, the same way you came. You do not need to book your ticket in advance. The Flybus operates for all arriving flights, and even in case of flight delays it will wait for the passengers.To get around in ReykjavíkCity /norsem/norsem2016/transportation/
  • 4. Pollution

    closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air. Stórhöfði - a seashore background station Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands /pollution-and-radiation/pollution/
  • 5. Early work and an overview of measurements

    Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138
  • 6. Early work and an overview of measurements

    Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138/
  • 7. ces_flyer_glacierssnowandice

    retreated and advanced in response to climate changes that are believed to have been much smaller than the greenhouse- induced climate changes that are expected during the next decades to century. The “Hydropower, snow and ice” work group of CES will analyse the effects of future climate change on glaciers and ice caps in Nordic countries and their implications for the hydrology of glacial rivers /media/ces/ces_flyer_glacierssnowandice.pdf
  • 8. Group4

    Abackcastingscenario was developed which built upon a set of normative assumptions.These normative assumptionsare intended toestablish a pathway for Finnish society to achieve a low-impact mobility system. The scenarios are designed for use internally within the Finnish Transport Agency to assist in long-range planning and strategic investment, explicitly grounded in adaptive management principles of multiple /media/loftslag/Group4.pdf
  • 9. Hare_2-participation

    08.03.06 Forum 4 15.06.05 KG Feb/March 05 Interviews Jan/Feb 05 Delivering the results: Bringing in other stakeholders Information provision and fun days Creating awareness 12 Bulgarian flood and drought management multi-level process (Daniell et al, 2010) Participatory Processes in Practice Infrastructure Initiatives Residential area Tow path School Park/ Bikers road/bridge UK: Canal /media/loftslag/Hare_2-participation.pdf
  • 10. Paper-Olafur-Rognvaldsson_91

    the opportunity to model river runoff and glacier mass balance both in the current climate and also in a hypothetical future climate based on the CE /VO climate change scenarios. The climate of Iceland is largely governed by the interaction of orography and extra-tropical cyclones, both of which can be described quite accurately by present day atmospheric models. As a result, dynamical downscaling /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

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