A chronology of glacier front fluctuations for northern Scandinavia derived from lichenometric and 14C-dates on moraines is compared with information about mass balance inferred from dendrochronology. Glacier advances not known from moraine stratigraphy in Sweden probably occurred around AD 1140 and AD 1240. -from Author
CITATION STYLE
Karlen, W. (1984). Dendrochronology, mass balance and glacier front fluctuations in northern Sweden. Climatic Changes on a Yearly to Millennial Basis. Proc. 2nd Nordic Symposium, Stockholm, 1983, 263–271. https://doi.org/10.1007/978-94-015-7692-5_29
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