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• 11. NOMEK09_Report

  Hermannsdóttir (Media) Sveinn Brynjólfsson (Avalanche) Theodor Freyr Hervarsson (Aviation) Guðrún Nína Petersen (Forecast errors) SMHI: Andreas Carlsson (Dynamics/NWP) Anna Eronn (Satellite) met.no: Bjørn Røsting (Dynamics) FMI: Vesa Nietosvaara (Online sessions and website) Elena Saltikoff (Radar-distans teaching) DMI: Claus Petersen (Slippery Roads) EUMETSAT: Jochen Kerkmann (Satellite /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf

• 12. ces-oslo2010_proceedings

  close to 2000 m a.s.l. Consequently, catchments having a hydrological regime influenced by snow and glacial melt show signs of sensitivity to temperature variations. The mean annual catchment-averaged temperature difference between the 25% warmest and 25% coldest years ranges from 1.5°C to 1.8°C depending on catchment. It is found that a mean annual temperature difference /media/ces/ces-oslo2010_proceedings.pdf

• 13. Kok_2-scenarios-lecture-2

  in development/policy • Plausible futures • No ‘desired’ future (no ‘doom or gloom’) EURURALIS: Model chain EU 25 arable and pasture land 160000 170000 180000 190000 200000 2000 2010 2020 2030 year # kh a A1 A2 B1 B2 EURURALIS: GTAP/IMAGE model EURURALIS: CLUE model Example 1c: MedAction Focus on participation and storylines Example 3: MedAction Land use change scenarios at various scales To better /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 14. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  Personality type differences between Ph.D. climate researchers and the general public: implications for effective communication C. Susan Weiler & Jason K. Keller & Christina Olex Received: 27 August 2009 /Accepted: 28 July 2011 / Published online: 2 September 2011 # The Author(s) 2011. This article is published with open access at Springerlink.com Abstract Effectively communicating the complexity /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 15. Monitoring of Hekla

  activity and possible hazards During the last millennium, Hekla has erupted 23 times, making it the third most active volcano in Iceland. Hekla's most recent eruption was in February 2000, when a 10 to 12-km-high plume of ash, gas and water vapour persisted for a couple of hours. The most recent major eruption of Hekla in 1947 created a volcanic plume that rose to about 30 km in the stratosphere /about-imo/news/monitoring-hekla

• 16. Reports and publications

  et al. 3 2005 Seismic hazard in the Hengill area based on the SIL earthquake catalogue - First results (PDF) Kristján Ágústsson, Páll Halldórsson 42 0,8 2005 A model of the release of the two June 2000 earthquakes based on all available observations (PDF) Sigurlaug Hjaltadóttir, Kristín S. Vogfjörð, Þóra Árnadóttir, Páll Einarsson, Peter Suhadolc 8 8,2 2005 /earthquakes-and-volcanism/reports-and-publications/

• 17. News

  News © Oddur Sigurðsson The western cauldron on 19 August 2000, shortly after a jökulhlaup in Skaftá /about-imo/news/bigimg/3142

• 18. Articles

  The glacier margin in the year 2000 is shown with a red curve. Spoken weather forecast Weather information via recorded messageTel: (+354) 902 0600 /weather/articles/bigimg/1618

• 19. An earthquake in South Iceland

  and Reykjavík. The fault on which the earthquake occurred is the same fault that gave rise to a magnitude 7 earthquake in August 1784. Yesterday's earthquake was not preceded by foreshocks and only a few aftershocks have been detected. This is the largest earthquake in this area since 2000, and the largest in the South Iceland lowland region (South Iceland seismic zone) since 2008. It is possible /about-imo/news/nr/2888

• 20. Refsgaard_etal-2007-Uncertainty-EMS

  BIOMATH, Ghent University, Gent, Belgium d Water Quality Modelling modelEAU, University Laval, Quebec, Canada Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007 Available online 27 April 2007 Abstract A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader water /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf