....................................................................................................................................... 9
Ágrip ......................................................................................................................................... 11
1 General introduction ........................................................................................................... 13
1.1 Main aim of the project
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
findings from various surveys
and studies, which highlight both the distinctiveness and some shared perspectives at a generalised
level. We reflect upon these in relation to trust and responsibility for climate change action, and risk
communication, supporting the call for discourses about climate change to also be situated in people’s
locality, as a means of increasing its saliency.
1/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com-
bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement
compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or
better than persistence, depending on catchment and lead time. Usually, persistence performs
better for T=1 day and then method 3
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf