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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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| Publicat a: | Nat Commun |
|---|---|
| Autors principals: | , , , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6105601/ https://ncbi.nlm.nih.gov/pubmed/30135494 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05814-0 |
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