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• 41. Bardarbunga_kafli20140825

  have extensive ice cover. The 2009 m high Bárðarbunga central volcano lies at the NW edge of the ice cap, with only its NW slopes ice free. It is dominated by a 80 km2 and up to 700 m deep ice-filled caldera. Bedrock rises to 1850 m in the northwest caldera rim and is lowest in a narrow gap the east rim where minimum elevation is 1350 m. The ice free fissure swarm north of Vatnajökull strikes /media/jar/Bardarbunga_kafli20140825.pdf

• 42. 2010_012rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 43. Water_resources_man_Veijalainen_etal

  Volume 24, Number 13 Water Resour Manage (2010) 24:3437–3459 DOI 10.1007/s11269-010-9614-z Climate Change Impacts on Water Resources and Lake Regulation in the Vuoksi Watershed in Finland Noora Veijalainen · Tanja Dubrovin · Mika Marttunen · Bertel Vehviläinen Received: 12 July 2009 / Accepted: 22 February 2010 / Published online: 24 March 2010 ³ Springer Science+Business Media B.V. 2010 Abstract /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 44. Factsheet_Bardarbunga_20141015

  Air quality:  Today (Wednesday) light easterly winds are expected. The gas pollution that has been hovering over the country as well as the gas erupted today will move slowly towards the west. The eastern part of Iceland will therefore be pollution free in the afternoon, but in most other parts of Iceland, pollution can be expected, and air quality can be poor in places. Tomorrow (Thursday /media/jar/Factsheet_Bardarbunga_20141015.pdf

• 45. Paper-Olafur-Rognvaldsson_91

  integration. Other investigators (e.g. Giorgi and Mearns, 1999) opt for longer integration times, emphasising the importance of the model to be free to develop its own internal circulations. Liang et al. (2004) used this approach when simulating precipitation over the U.S. during 1982–2002 using the MM5-based regional climate model CMM5. Several case studies investigating orographic forcing /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 46. 47th Nordic Seismology Seminar

  Reykjavík, which can be booked during the registration process. Of course, participants are free to book any other accommodation on their own.Other hotelsOther hotels in walking distance from the meeting venue, Grand Hotel, are for instance:Hotel Cabin ($$) Town House Guesthouse ($)Hilton Reykjavík Nordica ($$$)Hotel Lotus ($$) Galaxy Pod Hostel ($)The above accommodation, or any other of your own /norsem/norsem2016/accomodation/

• 47. Climate and Modeling Scenarios

  A. (2010b). 21st century changes in the European climate: uncertainties derived from an ensemble of regional climate model simulations. Tellus, published online. DOI: 10.1111/j.1600-0870.2010.00475. Ólafsson H, & Rögnvaldsson Ó. (2010). Regional and Seasonal Variability in Precipitation Scenarios For Iceland. Hydrology Research, in revision. Peltonen-Sainio, P., Hakala, K., Jauhiainen, L /ces/publications/nr/1680

• 48. Dyrrdal_Anita_CES_2010

  -08 – 225 stations Introduction Data & Methods Results 138 mutual stations Climate grids, 1x1 km (www.seNorge.no) Norwegian Meteorological Institute met.no Analysis • Mann-Kendall non-parametric trend test – Evaluate significance of trends in snow series • Linear trend test – Compare slopes to mean winter temperature • Analysis of correlation – Investigate snow parameters sensitivity /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 49. i-frame services

  The Icelandic Meteorological Office offers a service that allows web-masters to show weather information from IMO on their web-sites without effort. This service is free of charge, using the iframe technique. Two versions of iframes have been developed, one for station forecasts, text forecasts or observations, and another for weather elements (wind, temperature and precipitation forecasts /about-imo/the-web/iframes/

• 50. Adaptive management in relation to climate change

  to postdocs. If free places are available the course is also open to other professionals working in the subject area. Attending the course is free of charge. NONAM will provide accommodation for PhD students near the university free of charge. Participants are requested to cover travel expenses and daily allowances from their own funding. Other participants are requested to make their own /nonam/phd-summerschool/