Reconstructing climate from lake level changes

S. P. Harrison

Reconstructing climate from lake level changes

S. P. Harrison

Research output: Contribution to journal › Article › peer-review

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 language	English
Journal	LUNDQUA Thesis - Lund University, Department of Quaternary Geology
Volume	21
Publication status	Published - 1988

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title = "Reconstructing climate from lake level changes",

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",

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year = "1988",

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N2 - 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

AB - 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

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M3 - Article

AN - SCOPUS:0023685713

SN - 0281-3033

VL - 21

JO - LUNDQUA Thesis - Lund University, Department of Quaternary Geology

JF - LUNDQUA Thesis - Lund University, Department of Quaternary Geology

ER -

Reconstructing climate from lake level changes

Abstract

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