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in Holuhraun 31 August 2014. This photo is taken 31 January 2015 of the lava field, by then closely approaching 85 square kilometers. A month later, 28 February 2015, the eruption is declared over.
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/about-imo/news/bigimg/3097
and the groundwater module. The coupling
between both modules was done by a net boundary flux between the unsaturated zone and
the groundwater (Schulla & Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each
/media/ces/2010_016.pdf
Warning - high winds
20 - 28 m/s in the South and the West
24.2.2015
Bad weather is expected with poor travel conditions tomorrow, first in the south and west.
Northeast wind, 5 to 13 m/s and snow showers
/about-imo/news/nr/3090
in Vatnajökull is also being closely monitored (see plot 17 - 29 September), the last jökulhlaup from there having occurred in 2010.
Remark
29.9.2015 at 22:28: Floodwater is beginning to drain from the eastern Skaftá ice-cauldron, located beneath Vatnajökull. According to GPS measurements, the ice-surface above the lake began to subside late on 27 September. The rate of subsidence is increasing
/about-imo/news/nr/3199
Violent storm expected in the South
3.12.2015
A strong gale warning (average windspeed above 20 m/s) is effect in Iceland on Friday afternoon, and a violent storm (average wind speed, above 28 m/s) is expected in the southern
/about-imo/news/nr/3242
). Meteorological observations carried
out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor-
ology and surface energy balance data. Analysis ofthe first five years
/media/ces/GA_2009_91A_4_Andreassen.pdf
Simulation results
Hydropower
Thermal production
Energy balance
CO2-emissions
4 Summary and concluding remarks
Sintef Energy Research Quantitative system analysis 8 of 21
Introduction
Electricity system model
Simulation results
Summary and concluding remarks
Hydropower
Thermal production
Energy balance
CO2-emissions
Annual average in ow over the year, GWh
0 14 28 42 52
0
500
1;000
1;500
2;000
2;500
/media/ces/Mo_Birger_CES_2010.pdf
km south-southwest of the
eruption site at 15:00 GMT.
Lightning: Four lightning strikes detected over the summit of Eyjafjallajökull between
19:47 and 20:03 GMT on 28 April.
Noises: Booming sounds were reported yesterday evening, and again this morning,
from Selsund, located ~40 km north-northwest of the eruption site.
Additional note: 16:13 GMT: A sulphur smell was detected at 3
/media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf