Reconstructing climate from lake level changes

S. P. Harrison

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

The Late Quaternary geological record from lakes can be used to reconstruct changes in water depth and surface area. These changes reflect changes in the local hydrological balance. Regionally synchronous changes in the hydrological balance are climatically determined. -from Author

Original languageEnglish
JournalLUNDQUA Thesis - Lund University, Department of Quaternary Geology
Volume21
Publication statusPublished - 1988

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