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(18)O depletion in monsoon rain relates to large scale organized convection rather than the amount of rainfall
Oxygen isotopic variations in rainfall proxies such as tree rings and cave calcites from South and East Asia have been used to reconstruct past monsoon variability, mainly through the amount effect: the observed (18)O depletion of rain with increasing amount, manifested as a negative correlation of...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2014
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4092346/ https://www.ncbi.nlm.nih.gov/pubmed/25012535 http://dx.doi.org/10.1038/srep05661 |