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• 41. VAT_newsletter_2018_06

  Sporðar/te rmini (% ) 0 20 40 60 80 10 0 1930 1940 1950 1960 1970 1980 1990 2000 2010 2020 Hopa/Retreat Ganga fram Advance Engin breyting Stationary Gögn/Data: Jörfi/Icel. Glaciol. Soc. 1900 1920 1940 1960 1980 2000 2020 6 7 8 9 10 11 Hiti/ Tempe rature (°C ) Rúmmál/ Volume (km³ ) 50 55 60 65 70 Sumarhiti/Summer temperature Stykkishólmur ... 10−ára/year meðaltal/average Rúmmál/Volume /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 42. Moellenkampetal_etal-2010

  management actions. Stakeholder participation in water-planning and management processes is equally driven by supranational directives such as the European Union (EU)’s Water Framework Directive (EU 2000, 2002), national policies such as the Australian National Water Initiative (Council of Australian Governments 2004), and championed as a key underlying principle in integrated water resources management /media/loftslag/Moellenkampetal_etal-2010.pdf

• 43. 2010_012rs

  and providing early-warning mechanism information. Figure 1. Map showing SW-Iceland, the focus area within SAFER. Seismicity during 1997–2000, defining many of the already mapped faults, is shown colour coded according to age. Events with M>5 are shown as stars. The outline of the South Iceland Seismic Zone (SISZ) is shown with orange dashed lines. Test sites are marked on the map with letters K, H, Á /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 44. VI_2009_013

  mechanisms and the relationship between b-values and source depth is examined. During the analysis period, three major swarms were recorded. Two of the swarms, in 1994 and 1999–2000, occurred in the upper crust and were accompanied by crustal deformation. No uplift was detected during the third swarm, which occurred in 1996 near the crust mantle boundary, between 19 and 25 km depth /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 45. Adalgeirsdottir-etal-tc-5-961-2011

  of the model with past observations, it is used to simulate the future response of the glacier during the 21st century. The mass balance model was forced with an ensemble of temperature and precipita- tion scenarios derived from 10 global and 3 regional climate model simulations using the A1B emission scenario. If the average climate of 2000–2009 is maintained into the future, the volume /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 46. The weather in Iceland in 2019

  drought on record in Stykkishólmur. There are daily measurements there since 1856. The earlier record was 35 days (1931). Table 2: Precipitation overview 2019 from several stations. (1) Total precipitation (mm). (2) Percentage of the 1971 to 2000 average precipitation. (3) Percentage of the 10-year average precipitation (2009-2018). (4) Maximum 24-hr precipitation. (5) Number /about-imo/news/the-weather-in-iceland-in-2019

• 47. The weather in Iceland 2015

  in the Southwest. The weather in December was stormy. The year 2015 was the coldest in Iceland since 2000, but this period has generally been abnormally warm so the average temperature was close to the 1961-1990 mean. In most parts of the country the precipitation was well above normal. Temperature The average temperature in Reykjavík was 4.5°C, 0.2°C above the 1961-1990 mean. This is the 20th /about-imo/news/nr/3273

• 48. What is Bárðarbunga?

  is Bárðarbunga? Information on the central volcano 10.12.2014 There are about 30 known central volcanoes, or volcanic systems, in Iceland. Bárðarbunga, the second highest mountain of Iceland; ca 2000 meters above sea-level, is one of them. The volcano is placed /about-imo/news/nr/2968

• 49. The ice cap Snæfellsjökull is thinning rapidly

  Lowering of Snæfellsjökull. The year 2000 margin is shown with a red curve /weather/articles/nr/1618

• 50. The ice cap Snæfellsjökull is thinning rapidly

  Lowering of Snæfellsjökull. The year 2000 margin is shown with a red curve /weather/articles/nr/1618/