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....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
22N) from till
Illulisat DMI 50 10 105 497382 7681278 Ta 1.1.81 6.4.06
Station 437 ASIAQ 275 340 311 531316 7709513 Ta 5.9.83 1.6.06
Swiss Camp GC-net 1150 1115 780 566396 7719204 Ta, Sin 1.1.95 8.5.06
Crawford GC-net 2022 1795 1982 654464 7757807 Ta, Sin 24.5.95 2.5.06
2
2.3 RCM Data
Output from two RCMs is used: (1) the regional coupled ocean-atmosphere model RCAO
(Döscher et al., 2002) and (2
/media/ces/ces_geus_paakitsoq_full_report.pdf
operational cost, etc.) and the annual
revenues
• consider an appropriate discount rate and assess NPV (net present
value), IRR (internal rate of return), and net cash flows
• rank alternatives by score level
• SCBA: social CBA – total benefits -/- total costs for society, in this
case benefits and costs often don’t accrue (entirely) to the same
organisation due to the public nature of a project
/media/loftslag/Perrels-CBA.pdf
to highly
negative summer balances, but also lower bw than
the average for 1949–2006. Calculated change in
specific mass balance for a ±1°C change in air tem-
perature was ±0.55 m w.e., whereas a ±10 % in-
crease in precipitation represented a change of ±
0.20 m w.e. Model results further indicated that for
a 2°C warming, the ablation season will be extend-
ed by c. 30 days and that the period
/media/ces/GA_2009_91A_4_Andreassen.pdf
of Eyjafjallajo¨kul), Hveravellir (Hv; 641 m a.s.l., ca. 100 km north of Tindfjallajo¨kull
and Torfajo¨kull) and Ho´lar (Ho) in Hornafjo¨rdur (18 m a.s.l.). The plot shows the elevation distribution of the Eyjafjallajo¨kull, Tindfjallajo¨kull and
Torfajo¨kull ice caps as area (km2) per 10 m elevation interval.
Mass balance of three ice caps in southern Iceland S. Gudmundsson et al.
2
(page number
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
of how climate change will
impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources
and taking advantage of the local tempered climate for keeping the
supercomputer components cool, the running costs and CO2 footprint
will be kept to a minimum, saving tonnes of CO2 in line with the
four nations' efforts towards reaching Net/about-imo/news/joining-forces-in-weather-forecasting-and-climate-research