Transformation of ENSO‐related rainwater to dripwater δ18O variability by vadose water mixing
Speleothem oxygen isotopes (δ18O) are often used to reconstruct past rainfall δ18O variability, and thereby hydroclimate changes, in many regions of the world. However, poor constraints on the karst hydrological processes that transform rainfall signals into cave dripwater add significant uncertaint...
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| Main Authors: | , , , , , , , , , |
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| Format: | E-Article |
| Language: | English |
| Published: |
Wiley Online Library
2014
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| Subjects: | |
| Online Access: | http://ir.unimas.my/id/eprint/7016/1/Transformation%20of%20ENSO-related%20rainwater%20to%20dripwater.pdf http://ir.unimas.my/id/eprint/7016/ http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL061696/full |
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