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  • 1. Dyrrdal_Anita_CES_2010

    • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf
  • 2. norsem_martin

    a total of 325 well-constrained focal mechanisms were obtained using data from the permanent Icelandic SIL seismic network and a temporary network promptly installed in the source region following the main shocks, which allowed a high-resolution stress inversion in short time intervals during the aftershock period. More than 800 additional focal mechanisms /media/norsem/norsem_martin.pdf
  • 3. 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
  • 4. What is Bárðarbunga?

    in northwestern Vatnajökull ice cap and therefore covered with ice. The enormous size and nature of Bárðarbunga was not fully recognized until it was observed in 1973 on an image from a satellite, 800 km above Earth (see below). A caldera in the volcano's crown, 11 km long on the longer side, is covered with approximately 850 m thick glacial ice. Eruptions related to the central volcano can occur /about-imo/news/nr/2968
  • 5. Workshop on Jökulhlaup Hazards

    of over 800 inhabitants in the vicinity of the volcano. The resulting jökulhlaup drained from both the northern and southern flanks of the ice-cap, affecting an area of 57.5 and 1.5 km2, respectively. A second jökulhlaup on April 15 contained a large quantity of glacial ice; this flood propagated rapidly down the Markarfjót river, again necessitating a local evacuation. Workshop Goal The workshop /about-imo/news/nr/2251
  • 6. Grimsvotn_status_2011-05-24_IES_IMO

    and becoming darker in the process. Based on plume height, the estimated magma discharge rate equals 10- 70 tonnes/s of ash. A large part of Vatnajökull is covered by clouds and the eruption plume is not well defined in satellite images. South of Iceland images show visible ash extending over 800 km from the eruption site towards the south and southeast. Heading: A large part of the ash heads /media/jar/Grimsvotn_status_2011-05-24_IES_IMO.pdf
  • 7. Lawrence_Deborah_CES_2010

    ECHAM4/OPYC3 NorClim/HIRHAM 25x25 km 'Empirical Adjustment' to 1 x 1 km 100 150 200 250 300 350 400 450 500 550 600 650 700 750 800 850 900 1 10 100 1000 Return period (years) P e a k d a i l y d i s c h a r g e ( m 3 / s ) 1981-2010 GEV from annual max series 2021-2050 GEV from annual max series 2021 - 2050 Annual maximum series 1981 - 2010 Annual maximum series 1981-2010 200-year flood 2021 /media/ces/Lawrence_Deborah_CES_2010.pdf
  • 8. Pyroclastic flow

    a small amount of their heat to the atmosphere when the currents form. The temperature of the current can vary from 100°C up to 800°C. Depending on the density PDCs can be categorized into two groups. If the column contains a lot of solid material while it collapses it is called pyroclastic flows, however, if the quantity of solid material is low compared to the gases it is called a pyroclastic /volcanoes/volcanic-hazards/pyroclastic-flow/
  • 9. Factsheet_Bardarbunga_20150206

    has been detected in Bardarbunga since 8. January. • Around 20 earthquakes were detected in the dyke during the same period. The strongest one was M1.8. • GPS measurements near northern Vatnajokull glacier show continuing slow deflation towards Bardarbunga. • The highest levels of sulphuric dioxide since Tuesday, 3rd of February, 800 µg/m³ SO2 was measured in Vopnafjordur on Tuesday /media/jar/Factsheet_Bardarbunga_20150206.pdf
  • 10. Demers_Claude_CES_2010

    %), households (75%) and water (90%) heating and exports ConclusionAdaptationClimate & HydrologyContext Hydro-Québec and Climate Change Extreme Climate Events Saguenay (1996 : 800 M $) Flood 1: 11,000 years checkbldThe Great Ice Storm (1998 : 1,6 Billions $)1,5 millions customers without electricity for up to 30 days Ouranos: the Mission Ouranos’ mission is to acquire and develop knowledge on climate /media/ces/Demers_Claude_CES_2010.pdf

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