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How do tree-ring stable carbon and oxygen isotopes from different age groups respond to climate change? This study reveals that the stable carbon isotope from young trees have a large response to relative humidity variability, as a result, the stable carbon isotope from young trees have the potential to improve the relative humidity reconstruction. The study also explores the potential reasons of different climatic responses of stable carbon and oxygen isotope from different age groups.

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This page is a summary of: Age‐related climate response of tree‐ring δ 13 C and δ 18 O from spruce in northwestern China, with implications for relative humidity reconstructions, Journal of Geophysical Research Biogeosciences, April 2020, American Geophysical Union (AGU),
DOI: 10.1029/2019jg005513.
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