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  • 1. Dataseries and components

    Analysed components - IMO's research: Sulphur and salinity measurements: Precipitation: SO4-S, NO3-N, Cl, Na, Mg, K, Ca (mg/l) Precipitation: conductivity (µS/cm), quantity (mm), pH Aerosol: SO4-S, Cl, Na, Mg, K, Ca, Fe (µg/m3) Air: SO2-S (µg/m3) Heavy metals in precipitation: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/ml) Cl, NO3-N, SO4-S, Na, K, Ca, Mg, NH4-N, Br, F (µg/ml) conductivity (µS/cm /pollution-and-radiation/pollution/components/
  • 2. Grimsvotn_status_2011-05-23_IES_IMO

    in the northwest. A sample from Kirkjubæjarklaustur has been analyzed, which was taken around 1h on 22 May. The grains are glassy with micro crystals of plagioclase. Samples well sorted. Whole rock analysis: Basalt, with 50-51 Wt% SiO2 Leachate results: 5-10 mg/kg of waterdissolvable flour Grain size distribution: about 10 /media/jar/Grimsvotn_status_2011-05-23_IES_IMO.pdf
  • 3. QA on the eruption in Eyjafjallajökull 2010

    health, for example the respiratory system. The fluorine content is approximately 850 mg/kg according to chemical analysis carried out by the Institute of Earth Sciences, University of Iceland, on a sample taken 19 April. An earlier sample since 14 April only measured 25-35 mg/kg of fluorine because the water vapour from melting ice rinsed the ash. When the eruption progressed, water became less /earthquakes-and-volcanism/articles/nr/1880
  • 4. Pollution

    closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air. Stórhöfði - a seashore background station Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands /pollution-and-radiation/pollution/
  • 5. Alam_Ashraful_CES_2010

    Dominant height (m) Basal area just after thinning area threshold 60 80 100 120 Energy wood (Mg ha-1) 60 80 100 120 60 80 100 120 17 Findings: ecosystem CO2 balance 548.4 400 600 7.8 150.4 0 200 -200 O 2 m - 2 -390.86 -600 -400 g C O 1000 -800 -1097.6-1200 - Management Litter Humus 18 Emissions Capture Balance Conclusions • Large amount of unutilised energy biomass are available in Finland • Climate /media/ces/Alam_Ashraful_CES_2010.pdf
  • 6. VI_2015_006

    ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 7. Machguth_Horst_CES_2010

    experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf
  • 8. Joining forces in weather forecasting and climate research

    of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research
  • 9. Bardarbunga_kafli20140825

    systems in Iceland during the past 11 centuries: frequency, periodicity and implications. In Smellie JL and Chapman MG (eds): Volcano-Ice Interactions on Earth and Mars. Geological Society, London, Special Publications 202: 81-90. Larsen G, Guðmundsson MT, Einarsson P and Thordarson T. 2013. BÁRÐARBUNGA. In: Sólnes S, Sigmundsson F, Bessason B (eds.): Náttúruvá á Íslandi - Eldgos og /media/jar/Bardarbunga_kafli20140825.pdf
  • 10. Eyjafjallajokull_status_2010-05-07_IES_IMO

    recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

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