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note
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The authors express their warm thanks to the Abisko Research Station and their staff for much help and cooperation Particular thanks go to many other colleagues for reports of observations in connection with extreme erosional events, e.g. B Seyffarth, Oslo, D Scherer and M. Gude, Basel R Lundqvist, A. Nordin, H. Vedin, L. and Å. Frolander provided us with data and observations on Mt. Fulufjäll.
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