a complex policy matrix, including different social, cultural
and economic value considerations; and 5) participant observation, with 2-3 month site visits to the
respective planning agencies and departments in the case cities, Copenhagen and Portland.
Topics for the review discussions:
My theoretical frame is built upon cumulative prospect theory (Kahneman and Tversky), focusing on two key
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
It is updated more often if needed. The forecast is made for three days, and a frame identifies the current day.
More about the bulletin
The bulletin is made according to European standards, using a standardized danger rating system of EAWS (European Avalanche Warning Services). In May 2018 the visualization of the bulletin was changed from what it was before according to EAWS standards
/avalanches/forecast/help
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/media/ces/2010_017.pdf
) in 1956. During that time that ambitions of utilizing hydropower had changed from providing the public and
the sectors with electricity to aim for a large-scale utilization of hydropower for energy intensive industries. This came
to fruition in 1969 with the first aluminium smelter in Iceland. Today, energy intensive industry matches fisheries as a
key income sector for Icelandic society.
During
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
The hydrological simulations were performed with the Wa-
tershed Simulation and Forecasting System (WSFS) developed
and operated in the Finnish Environment Institute (Vehviläinen
et al., 2005). The WSFS is used in Finland for operational hydrolog-
ical forecasting and flood warnings (www.environment.fi/water-
forecast/), regulation planning and research purposes
(Vehviläinen and Huttunen, 1997
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
.................................................................................................................... 7
2 Data and methods ........................................................................................................... 8
2.1 Data and time frame .............................................................................................. 8
2.2 Domain and spatial resolution
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
than can be expected to originate from the cauldrons, three to four times the wa-
ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has
been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be
2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich
groundwater from the glacier comes from the cauldrons
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf