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• 41. Lettenmaier_Dennis_CES_2010pdf

  Dennis P. Lettenmaier Department of Civil and Environmental Engineering University of Washington Conference on Future Climate and Renewable Energy: Impacts, Risks, and Adaptation Oslo June, 1, 2010 Runoff projections and impacts on water resources Outline of this talk 1) Projected runoff changes over the next century – the global and continental picture 2) Downscaling to the regional /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 42. 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

• 43. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 44. Perrels-CBA

  26.8.2011Adriaan Perrels/IL 6 Review of climate change effects in built-up areas (1) Source: IPCC 4AR_2 Source: IPCC 4AR_2 26.8.2011Adriaan Perrels/IL 7 Source: IPCC 4AR_2 Review of climate change effects in built-up areas (2) 26.8.2011Adriaan Perrels/IL 8 Cost-benefit analysis – the basics 1 • CBA: • assess for the estimated lifetime of a project the annual expenditures (investment funding cost /media/loftslag/Perrels-CBA.pdf

• 45. 2010_003rs

  ..................................................................................................................... xv Acknowledgements .......................................................................................................... xvii 1 Introduction ..................................................................................................................... 1 1.1 Tectonics /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 46. VI2010-006_web

  Veðurstofu Íslands Halldór G. Pétursson, Náttúrufræðistofnun Íslands H æ t t u matsnefnd Akureyrarbæjar 4 Efnisyfirlit 1 Inngangur 7 1.1 Starf hættumatsnefndar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.2 Vinnuferli Veðurstofu Íslands . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 1.3 Efnisatriði og kaflaskipting /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 47. Hofsjökull ice cap gains mass

  and Drangajökull ice caps. All ice caps in Iceland have been retreating rapidly and losing volume since 1995, but in 2015 the Hofsjökull ice cap in the central highlands displayed positive mass balance. The equilibrium line altitude on the ice cap moved to a location 150 - 200 below the long-term average. This change is due to high precipitation in the winter of 2014 - 2015 and low ablation /about-imo/news/nr/3229

• 48. 2010-05-02_En-IES_IMO

  the eruption site. Plume track visible at least 200 km from the eruption site on MODIS (12:35 GMT) and EUMETSAT (17:15 GMT) satellite imagery. Colour: Dark grey (ash) clouds observed over the eruptive site. White (steam) plumes rising from Gígjökull, north of the eruption site. Tephra fallout: Moderate ash-fall reported in the village of Vík (12:00 GMT), located 40 km south-east /media/jar/2010-05-02_En-IES_IMO.pdf

• 49. Eyjafjallajokull_status_2010-04-30_IES_IMO

  :00 GMT a flood was detected leaving the Gígjökull lake basin. The flood reached a maximum discharge about two hours later at the old bridge over Markarfljót, ~18 km downstream. The flood was comparable in size to yesterday's gauged flows. At 14:00 GMT, meltwater flow beneath the bridge was ~200 m3 s–1. Discharge from Gígjökull decreased during the afternoon. Steaming blocks /media/jar/Eyjafjallajokull_status_2010-04-30_IES_IMO.pdf

• 50. The weather in Iceland 2014

  above the 1961 to 1990 average. It was also the second warmest year in Akureyri (since the start of the series in 1881), only 1933 was warmer. The temperature was far above normal until October. Reykjavík blue, Akureyri red. November was also extraordinarily warm, but December considerably colder and the coldest month of the year. Table 1. Temperature in 2014 station temp °C dev. 1961-1990 /about-imo/news/nr/3082