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1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

2. Refsgaard_1-Welcome

– Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf

3. Daniell_etal-2010

and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

4. Sea ice in December 2010

was closest to land 21.7 nm from Horn, 25.3 nm from Straumnes and 43.6 nm from Barði. The tongue which stretched eastwards, north of Iceland, was scattered. Only towards the west, the ice was quite dense. Large icebergs were seen in the area. On the 10th, IMO issued a warning saying that the ice edge might move closer to land in the next 24 hrs. The Coast Guard did an ice survey flight on the 12th /sea-ice/monthly/2010/nr/2347

5. Articles

6. norsem_martin

for the time period 2001–2009, obtained from the permanent SIL network, were analysed to study stress changes associated with the main shocks. Results reveal a coseismic counter-clockwise rotation of the maximum horizontal stress of 11 ± 10° (95 per cent confidence level) in the main rupture region. From previous fault models obtained by inversion of geodetic data, we estimate a stress drop /media/norsem/norsem_martin.pdf

7. ces-oslo2010_proceedings

change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

8. New web for mobiles

This is the most frequently accessed information on our main web and should be of use to travellers and tourists who do not have access to the internet, except via their mobiles. In July this service will be extended. Wind, temperature and precipitation forecasts will be available, as well as information on recent earthquakes and the level of some main rivers. With further improvement, IMO's mobile /about-imo/news/nr/1612

9. News

10. News

Met Office's main weather station for Iceland 1881-1920, then a manned station of the Icelandic Met Office, and now an automatic weather station. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/bigimg/3273

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