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• 71. ces-glacier-scaling-memo2009-01

  of the area and mean elevation for the ice-free and glaciated parts of each elevation band or grid cell. The areas are denoted by ai and gi, and the elevations by zi and yi, for the ice-free and the ice-covered areas, respectively. At the end of each hydrological year, the hydrological model will provide a simulated value for the total mass balance of each glacier group within the watershed, DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 72. Journal_of_Hydrology_Veijalainen_etal

  precipitation and time of year (an index for available net radiation) (Vehviläinen and Huttunen, 1997). This equation has been calibrated and verified against observations of Class A pan evaporation values (Vehviläinen and Huttunen, 1997). The actual evaporation is calculated from potential evapora- tion and the soil moisture deficit. The changes in temperature and precipitation affect /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 73. Hydropower - Glacier, Snow and Ice

  of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.). Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1. Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I /ces/publications/nr/1940

• 74. PhD_course-Programme_26Aug2011-final

  of a large-scale agricultural catchment. WATER RESOURCES RESEARCH, VOL. 45, W00A15, doi:10.1029/2007WR006760 Kok K, Veldkamp TA (2011) Scale and governance: conceptual considerations and practical implications. Guest editorial special feature Scale and Governance. Ecology and Society 16(2): 23. [online] URL: http://www.ecologyandsociety.org/vol16/iss2/art23/ Kok K, van Vliet M, Bärlund I /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 75. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 76. Cooperation is a must for adaptation to and

  the long-term background warming. Mild and snow-free conditions in winters will reduce the number of extreme cold events. For summers more heat waves and droughts may be expected as a result of a longer season with high temperatures in combination with relatively small increases, or even regional decreases, in precipitation. Other, more uncertain impacts on the large-scale circulation /about-imo/news/cooperation-is-a-must-for-adaptation-to-and-mitigation-of-climate-change

• 77. The weather in Iceland in 2016

  heavy precipitation for a period in the South and West, the monthly totals were record high at a few stations. The month was totally frost-free in most coastal areas, which is unusual. NovemberThe month was a warm one with heavy precipitation and the weather was favourable but dark and gloomy. DecemberThe warm weather continued until just before Christmas, in the East this was the warmest /about-imo/news/the-weather-in-iceland-in-2016

• 78. Glacial outburst floods

  from ice-dammed marginal lakes. Such lakes often form when an outlet glacier closes off an ice-free side valley. Grænalón is an Icelandic example of such a lake.Jökulhlaups from supraglacial lakes which have formed by accumulation of meltwater in depressions on the surface of the glacier. Such floods are generally small in Iceland but can be of substantial magnitude on the Greenland ice /volcanoes/volcanic-hazards/glacial-outburst/