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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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Bibliographic Details
Main Authors: Jessica W, Moerman, Kim M, Cobb, Judson W, Partin, A Nele, Meckler, Stacy A, Carolin, Jess F, Adkins, Syria, Lejau, Jenny, Malang, Brian, Clark, Andrew Alek, Tuen
Format: E-Article
Language:English
Published: Wiley Online Library 2014
Subjects:
GE Environmental Sciences
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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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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