least-squares line derived by Bahr and others (1997) for 144 glaciers not
including ice caps. The figure also shows numerical simulations of the volume and area for
southern Vatnajökull, Langjökull and Hofsjökull (Jóhannesson and others, 2007) for a warm-
ing climate scenario developed as a part of the Climate and Energy (CE) project (Fenger, 2007).
Symbols denote pairs of volume and area with 50
/media/ces/ces-glacier-scaling-memo2009-01.pdf
and the responder. All subjects made decisions under both roles before
knowing the actual role they were assigned. At the end of the session, the program ran-
domly allocated a role to each subject and payoffs were determined accordingly. Half of
the subjects were allocated to be senders and half responders. All subjects were matched in
pairs, with a sender and a responder in each pair.
As a sender, each
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
-out group, assuming the initiative is at the public
side.
Red: inside transport system; blue: direct impact on size & quality of demand for road vehicle
movements; grey: auxiliary services that strongly interact with effects of CC.
Various possible effects of climate change on road infrastructure and its users
The expected effects of a changing climate in Nordic countries imply among others
/media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
the pairs of catchments used to develop and validate the index flood
models with simulated series are of relatively similar size, while some of the other catchments
are much larger, and so is their index flood. Consequently, the RMSE obtained when validating
the method with the simulated series are usually lower than those obtained with the observed
series from the other catchments.
When the best index
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf