2015, 2025, 2035 and 2050
North (Blanda) East (Karahnjukar) South (Thorisvatn)
Change in average inflow to the main storage reservoirs
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•Change in temperature
• 0.75 °C/100y 1950-1975
• 1.55
/media/ces/Linnet_Ulfar_CES_2010.pdf
and insignificant
crustal movements north of Vatnajökull around the dyke.
Air quality in urban areas in the East of Iceland:
o High air pollution was detected yesterday in Egilsstaðir and Reyðarfjörður.
Forecasts indicate that the gas cloud will blow towards the north in the next
24 hours. High concentrations of sulphuric gases can be expected in
Mývatnssveit, Kelduhverfi, Tjörnes, Húsavík
/media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf
EA Analyse A/S and Optensys
Energianalys will forecast energy system variables, while SINTEF Energy Research will make
assumptions for the energy system in different cases, include new inputs in the EMPS model and
carry out simulations.
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/media/ces/esa_flyer_new.pdf
course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
6
Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired
adaptation planning cycle for road transport (at national strategic / tactical level)
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/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
observed, but steam rises from
the lava.
Air quality in urban areas in the East of Iceland:
o Forecasts indicate that high concentrations of sulphuric gases may be
expected in the northern part of the Eastern fjords, Fljótsdalur, Hérað,
Jökuldalur, and Vopnafjörður. High concentrations could occur in other areas
as well. People who feel discomfort are advised to stay indoors, close the
windows
/media/jar/Factsheet_Bardarbunga-140911.pdf
TS.1b, TS.2b}
Global anthropogenic GHG emissions
F-gases
CO2 from fossil fuel use and other sources
CH4 from agriculture, waste and energy
CO2 from deforestation, decay and peat
N2O from agriculture and others
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/media/loftslag/IPPC-2007-ar4_syr.pdf
the eruption site.
Four scenarios are likely:
o The migration of magma could stop, resulting in a gradual reduction in
seismic activity and no further eruptions.
o The dike could reach the Earth’s surface causing another eruption, possibly
on a new fissure. Lava flow and (or) explosive activity cannot be excluded.
o The intrusion reaches the surface and another eruption occurs where
/media/jar/Factsheet-Bardarbunga-140903.pdf
by season (%) between
1991-2007 and 1961-1990 in the Baltic countries
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/media/ces/ces_SA_group_flyer_new.pdf
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
& Togeby, M. (2007). Statistical Analysis. In: J. Fenger (Ed.) Impacts of Climate Change on Renewable Energy Sources: Their role in the Nordic energy system, Nord 2007:003, 154-174.
Mo, B., Wolfgang, O. & Styve, J. (2010). ”The nordic power system in 2020 - Impacts from changing climate conditions”, Conference on future climate and renewable energy: Impacts, Risks and Adaptation, 31.May-2 June 2010
/ces/publications/nr/1937