Reconstructing climate from lake level changes

S. P. Harrison

    Research output: Contribution to journalArticlepeer-review

    4 Citations (Scopus)


    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
    Publication statusPublished - 1988


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