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31. The Icelandic glaciers weighed from space

glacier downwasting indicated by the traditional mass balance measurements that show that the volume of the glaciers has been reduced by more than 200 km³ in total since 1995, see fig. 3, as described in a new scientific publication in the journalGeophysical Journal International . Since the measurements determine changes in the total mass of the glaciers, one may say that the glaciers have /about-imo/news/the-icelandic-glaciers-weighed-from-space
32. The weather in Iceland in 2050

stocks. The acidification of the ocean may also adversely impact ocean food webs, with possible consequences on fisheries. Iceland's ice caps have been melting and will continue to do so. According to scientific estimate, they will almost disappear in the next 200 years. Many of these changes can already be seen, for instance: The tiny ice cap Ok, west of Langjökull, has changed beyond /about-imo/news/nr/2989
33. Instructions for weather radar pages

the earth's surface. At a distance of 200 km from the weather radar the laser beam does not detect signals which are under 4000 m from the earth's surface. Low clouds, for example fog clouds, close to the weather radar do not appear on the image; they lie so close to the earth's surface that they are not detected. The utility of these images is most when monitoring precipitation from the south /weather/articles/nr/1221
34. Daily_status_report_200814

cloud. Lightning No eruption and no eruption cloud. Noise No eruption and no eruption cloud. Meltwater No eruption. Daily measurements of water samples from Upptyppingar on Jökulsá á Fjöllum have shown a stable conductivity of 200 µS/cm since Sunday. Conditions at eruption site No eruption. Seismic tremor No sign of harmonic (volcanic) tremor detected. Earthquakes The earthquake swarm that began on 16 /media/jar/Daily_status_report_200814.pdf
35. Eyjafjallajokull_status_2010-04-26_IES_IMO

observations. Radar images show continuous build-up of a tephra crater/cone in the northern ice cauldron. The diameter of the crater is 200 m and the height of the crater cone is 150 +- 20 m. Seismic tremor: Intensity comparable to the last three days of eruptive activity Earthquakes: Ml 1.7 earthquake detected ~8 km east of the eruption at 16:18 GMT GPS deformation: Horizontal displacement towards /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf
36. Eyjafjallajokull_status_2010-05-18_IES_IMO

the center of Eyjafjallajökull volcano together with subsidence. Overall assessment: A powerful explosive eruption is ongoing and theheight of the suggests that the eruption rate is over 200 tonnes/s. Fallout of tephra has been detected mainly to the northeast of the volcano, with recorded fallout on the northeast coast. Some tephra dispersion towards west in the afternoon. /media/jar/Eyjafjallajokull_status_2010-05-18_IES_IMO.pdf
37. Eyjafjallajokull_status_2010-06-04_IES_IMO

In the main crater steaming is still active. However, intensity of the steam is considerable smaller than it was last week. Steam rises some 200 to 400 m above crater rim. South of the volcano winds 8-13 m/s are blowing from the east today. Heading: N/A Colour: N/A Tephra fallout: Widespread drifting of existing ash in south- and southwest Iceland, both yesterday and today. Lightning /media/jar/Eyjafjallajokull_status_2010-06-04_IES_IMO.pdf
38. Factsheet-Bardarbunga-140907

not decreased. Magma flow is between 100 and 200 m3/s. The lava advances by about 1 km/day and its area yesterday afternoon was around 16 km2. o The eruption sites are the same as before. The eruptive intensity on the southern fissure that opened on Friday is much less than on the northern fissure that has been active since the beginning of the eruption. o The lava tongue now extends 11 km /media/jar/Factsheet-Bardarbunga-140907.pdf
39. Mo_Birger_CES_2010

3;000 3;500 4;000 4;500 5;000 Week In ow , GW h Sweden Reference Echam Hadam 0 14 28 42 52 0 1;000 2;000 3;000 4;000 5;000 6;000 7;000 8;000 9;000 Week In ow , G W h Norway 0 14 28 42 52 0 200 400 600 800 1;000 1;200 Week In ow , G W h Finland Sintef Energy Research Quantitative system analysis 9 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks /media/ces/Mo_Birger_CES_2010.pdf
40. Alam_Ashraful_CES_2010

dimension to current mgt. as it utilises the opportunity provided by the surrounding environment  Energy biomass production 7 What are the challenges?  EU is committed to raise the share of renewable energy to 20% by 2020  This target for Finland is 38% by 2020  The production of energy biomass to substitute fossil fuels I 2006 21 il 3 (46 TWh) f bi d i  n 200 , 21 m . m o energy /media/ces/Alam_Ashraful_CES_2010.pdf