Climatologic and hydrologic influences on the oxygen isotope ratio of tree cellulose in coastal southern California during the late 20th century

The oxygen isotope ratio (δ18O) of precipitation in continental, midlatitude regions is a complex measure of atmospheric dynamics and regional climate variability and can be preserved in geologic archives. However, continuous modern observations of precipitation δ18O in many midlatitude regions, par...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Lisa Kanner, Nikolaus Buenning, Lowell Stott, Dave Stahle
Format: Article
Language:English
Published: Wiley 2013-10-01
Subjects:
Online Access:https://doi.org/10.1002/ggge.20256