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
mean surface air temperature anomalies ....................................... 28
14 Surface air temperature anomalies over Scandinavia ...................................... 29
15 Composite mean precipitation anomalies..................................................... 30
6
1 Introduction
Extratropical low-pressure systems, persisting for at least a few days, have long been recognised
as one
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
%) and man-made disasters (46%). However, significant differences
were evident between responses in the former EU-15 and the newer 10 MS. On
average, climate change was the most mentioned environmental concern in the
EU-15 (47%), whereas it was only mentioned by 34% of respondents in the newer
10 MS (e.g. 28% in Latvia, 32% in Hungary but 43% in the Czech Republic). This
average is below the lowest
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
balance data from all the ice caps.
REFERENCES
Björnsson, H., Pálsson F., Guðmundsson M. T. and Haraldsson H. 1998. Mass
balance of western and northern Vatnajökull, Iceland, 1991–1995, Jökull, 45,
35–58.
Björnsson, H., Pálsson F. and Haraldsson H. 2002. Mass balance of Vatnajökull
(1991–2001) and Langjökull (1996–2001), Iceland. Jökull, 51, 75–78.
Bromwich, D. H., Bai L. and Bjarnason G. G. 2005
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf
Dubel A, Sendzimir J (2011) Combining participative backcasting and explorative scenario development: Experiences from the
SCENES project. Technological Forecasting and Social Change 78(5): 835-851. doi:10.1016/j.techfore.2011.01.004
Moellenkamp, S., Lamers, M., Huesmann, C., Rotter, S., Pahl-Wostl, C., Speil, K., Pohl, W. (2010). Informal participatory platforms for adaptive management –
insights
/media/vedurstofan/PhD_course-Programme_26Aug2011-final.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