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• 11. Cradden_Lucy_CES_2010

  -90 (Amps) 470 480 490 500 510 520 530 540 550 560 570 Rating at 90% for 2050s period (Amps) 470 480 490 500 510 520 530 540 550 560 570 June 2010 14 Time series • Using the UKCP09 ‘weather generator’ to determine temperature and solar radiation for control period and future scenario: 2050s, medium emissions 0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 450 475 500 525 550 575 600 625 650 675 700 725 /media/ces/Cradden_Lucy_CES_2010.pdf

• 12. Moberg_Anders_CES_2010

  www.millenniumproject.net Climate proxy data - far less accurate than meteorological observations - decreasing data network back in time - less information about paleohydrology than paleotemperature IPCC 2007, Fig. 6.11 Northern Hemisphere mean temperature last 1500 years Mann et al. Science 2009, 326, p.1257, Figs. 1-2 Stockholm winter/spring temperatures last 500 years Data: Leijonhufvud et al. Climatic /media/ces/Moberg_Anders_CES_2010.pdf

• 13. VI_2016_006_rs

  seen from northeast. The debris piles in the foreground are at the bottom of the inner cirque. Photograph: Árni Hjartarson. Two cirques called Efri-Botnar (also called Dagmálabotnar) are situated at an elevation 400– 500 m a.s.l. to the southwest of Strandartindur. The outer cirque is located between Strandar- tindur and Miðtindur while the inner one is between Miðtindur and Innri-Strandartindur /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 14. IPPC-2007-ar4_syr

  period in the last 500 years and likely the highest in at least the past 1300 years. {WGI 6.6, SPM} 2 Likelihood and confidence statements in italics represent calibrated expressions of uncertainty and confidence. See Box ‘Treatment of uncertainty’ in the Introduction for an explanation of these terms. 3 Excluding tsunamis, which are not due to climate change. Extreme high sea level depends /media/loftslag/IPPC-2007-ar4_syr.pdf

• 15. ces-oslo2010_proceedings

  an impact on the snowpack and the resulting snowmelt rate and timing for all catchments. The sensitivity of the snowmelt to temperature variations depends on catchment altitude. The catchments located at lower elevations are most affected by temperature increase. Those at higher altitudes are also affected since the altitude range in Iceland is moderate, with an average of 500 m a.s.l and a maximum /media/ces/ces-oslo2010_proceedings.pdf

• 16. Factsheet-Bardarbunga-140901

  -area. This corresponds to a magma discharge of 300 to 500 cubic metres per second. From observations yesterday evening, the volume of erupted lava is between 16 and 25 million cubic metres. The eruption has not created any ash-fall. Gas and steam rises to a couple of hundred metres above the eruption site, extending up to 1,200 m downwind. In connection with the FUTUREVOLC project, a gas /media/jar/Factsheet-Bardarbunga-140901.pdf

• 17. Map of the glaciers of Iceland

  the IMO has for some time worked on the publication of a map of the glaciers of Iceland, released in May 2013. The purpose of the edition is to make available a detailed map of the glaciers in the country and draw attention to the huge ongoing changes in Iceland's glaciers that occur as a result of climate change. The map is on a scale of 1:500 000 and shows the outlines of glaciers in Iceland /about-imo/arctic/map-of-glaciers/

• 18. Glaciologists meet in Iceland

  changes in a wider societal context were also on the agenda. Participants visited the geothermal baths of Krauma and the 500 m long man-made ice tunnel in Langjökull ice cap, pictured above. (Photo: IMO) A 2-day beginner Elmer/Ice course took place in Reykjavík prior to the Nordic Branch meeting, for researchers and students aiming to start working with Elmer/Ice. The course was sponsored /about-imo/news/nordic-glaciologists-meet-in-iceland

• 19. VONA message

  as the impact on air traffic is considered negligible at this stage. Cloud height:Rough estimates indicate the gas plume reaches between 500 m and 1 km. Other cloud information:Gas release is ongoing from the fissure. No ash emission. Remarks:More information about this volcanic system is available at: https://icelandicvolcanos.is/?volcano=KRY /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 20. Grimsvotn_status_2010-11-02_IES_IMO

  Grímsvötn, but the rate of discharge increase has slowed. At 09:30 GMT today, discharge was gauged at 1,200 m3/s. Electrical conductivity has increased to 500 µS/cm. Increased electrical conductivity in the Súla river suggests that a small volume of geothermal water is draining from the western side of the Skeiðarárjökull glacier. Seismic tremor: High-frequency seismic tremor /media/vatnafar/flod/Grimsvotn_status_2010-11-02_IES_IMO.pdf