Precession-band variance missing from East Asian monsoon runoff

Speleothem CaCO(3) δ(18)O is a commonly employed paleomonsoon proxy. However, inferring local rainfall amount from speleothem δ(18)O can be complicated due to changing source water δ(18)O, temperature effects, and rainout over the moisture transport path. These complications are addressed using δ(18...

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Detalles Bibliográficos
Autores principales: Clemens, S. C., Holbourn, A., Kubota, Y., Lee, K. E., Liu, Z., Chen, G., Nelson, A., Fox-Kemper, B.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6105601/
https://www.ncbi.nlm.nih.gov/pubmed/30135494
http://dx.doi.org/10.1038/s41467-018-05814-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6105601/
https://www.ncbi.nlm.nih.gov/pubmed/30135494
http://dx.doi.org/10.1038/s41467-018-05814-0

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