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Can tree-ring isotopes (δ 18 O and δ 13 C) improve our understanding of hydroclimate variability in the Columbia River Basin?
Can tree-ring isotopes (δ 18 O and δ 13 C) improve our understanding of hydroclimate variability in the Columbia River Basin?
2015
A. Z. Csank
E Wise
S. A. McAfee
Keywords:
Isotope
Dendrochronology
Geography
Climatology
Drainage basin
Physical geography
Global change
Correction
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