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  • 11. Kjellstrom_Erik_CES_2010

    ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf
  • 12. norsem_asdis

    of Eyjafjallajökull, at approximately 5-7 km depth. The high velocity zones are elongated in the east-west direction, in line with geological surface features and are separated by a zone of relatively lower velocity (3.0 km/s), where earthquakes prior to and during the 2010 summit eruption were located. The high velocity zones most likely correspond to intrusive bodies similar to those previously imaged /media/norsem/norsem_asdis.pdf
  • 13. Savolainen_Ilkka_CES_2010

    reduction scenarios for limiting the emission by 50% and by 85% corresponding the overlimit emissions and underlimit emission for a temperature rise level of 2 C. 903/02/2010 WEO 2009 1003/02/2010 IPCC Special Report on Renewable Energy Sources and Climate Change Mitigation (SRREN) 1) Introduction (Renewable energy and climate change) (5% share of the whole report) 2) Bioenergy (15 %) 3) Direct /media/ces/Savolainen_Ilkka_CES_2010.pdf
  • 14. Factsheet_Bardarbunga_20150130

    as the volume of the lava field at Holuhraun. The red dotted line is an exponential curve used to estimate the diminishing flow of lava from the Holuhraun eruption and estimate when the lava flow will go below 5 m3/s. If the diminishing activity follows this trend then the eruption might come to an end anywhere between June 2015 and April 2016. NATIONAL COMMISSIONER OF THE ICELANDIC POLICE /media/jar/Factsheet_Bardarbunga_20150130.pdf
  • 15. Significant ground

    Peninsula, between Fagradalsfjall and Kleifarvatn - the largest of which was a magnitude 5.6 earthquake in the vicinity of Núpshíðarháls, which occurred at 13:43 on 20th October. The maps displayed here show ground deformation associated with movement on faults during the period 16th-22nd October.The large signal shown in the vicinity of Skolahraun represents movement of up to 5 cm /about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake
  • 16. Instructions on using wind, precipitation and temperature forecasts

    shows the direction of the wind, which blows toward the point of the barb. Wind-speed is symbolized by diagonal lines at the end of the barb; for instance, a short line represents 2.5 m/s, a long line 5 m/s and a triangle represents 25 m/s. Mean sea level pressure is shown in solid lines, the contour interval is 2 hPa. The sliding bar below the map is used to change the validity time /weather/articles/nr/1211
  • 17. IPPC-2007-ar4_syr

    forcings. Decadal averages of observations are shown for the period 1906-2005 (black line) plotted against the centre of the decade and relative to the corresponding average for the 1901-1950. Lines are dashed where spatial coverage is less than 50%. Blue shaded bands show the 5 to 95% range for 19 simulations from five climate models using only the natural forcings due to solar activity /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 18. 2010_003rs

    is N197°E. The J21 fault, on the other hand, is more linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9 km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000 activity have also been mapped, including the fault planes of three M~5 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
  • 19. Uplift signal detected in Askja volcano

    East and Up components over the period 27 July – 2 September 2021. The station, which is located close to the center of the inflating area, shows that the uplift started between the end of July and beginning of August (mainly visible in the Up component) and it is still ongoing (2. Sept 2021). The dashed red line indicates the rise speed that is assessed to be ~5 cm /month /about-imo/news/uplift-signal-detected-in-askja-volcano
  • 20. VI_2022_006_extreme

    – 1987, bottom). The vertical red lines indicate the start date of the melt season as retrieved by the first filtering method. 13 Figure 5 – Evolution of the snowpack (black line), cumulative melting (dashed blue line), and daily runoff (grey bars) for Hágöngulón (year 1986 – 1987, top; year 1984 – 1985, bottom). The vertical red lines indicate the start date of the melt season /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

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