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• 11. tj_hofsj-langj-ces2010-video

  Year: 1990 Year: 1995 Year: 2000 Year: 2005 Year: 2010 Year: 2015 Year: 2020 Year: 2025 Year: 2030 Year: 2035 Year: 2040 Year: 2045 Year: 2050 Year: 2055 Year: 2060 Year: 2070 Year: 2075 Year: 2080 Year: 2085 Year: 2090 Year: 2095 Year: 2100 Year: 2100 /media/vedurstofan/utgafa/hlidarefni/tj_hofsj-langj-ces2010-video.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. Keskitalo_et_al-MLG_and_adaptation_FINAL

  such processes as lobbying from influential regional or local actors (Rhodes 2000). Initiatives may also manifest at the national level as a result of state commitments under international conventions that bind states to decision-making that originates elsewhere. Within the EU context, states have also agreed to be bound by EU legislation, so that directives taken on the EU level directly /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 14. 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

• 15. 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/

• 16. News

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

• 17. 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

• 18. 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

• 19. norsem_ingi

  1991 to 2000 are being analyzed. The period includes two large earthquakes in year 2000, both of them of the magnitude 6.5. The analysis involves improving earthquake locations in order to determine if in situ changes do exist in the area (down to ~0.5% significance level), with the ultimate goal of locating them at relatively high spatial resolution (~10x10x3 km3). With such a high /media/norsem/norsem_ingi.pdf

• 20. Journal_of_Hydrology_Veijalainen_etal

  and to evaluate the need for further and more detailed case studies. 2. Study area 2.1. Climate and hydrology in Finland The climate of Finland is controlled by several factors such as latitudinal gradient, maritime climate from the Atlantic Ocean and continental climate from Eurasia, the Scandinavian mountain range and the Baltic Sea (Atlas of Finland, 1987; Käyhkö, 2004). In 1971–2000 the average /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf