and CNES, n.d.;
National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional
altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein
et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea
level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013
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Roald, L.A. and Engen-Skaugen, T.
Projected effects of climate change on the hydrology of Norway ........................................................................ 80
Duncan, N.J., Harrison, G.P. and Wallace, A.R.
Modelling the Scottish hydropower resource ........................................................................................................ 82
Einarsson, B
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