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Tropical mountain ice core δ(18)O: A Goldilocks indicator for global temperature change
Very high tropical alpine ice cores provide a distinct paleoclimate record for climate changes in the middle and upper troposphere. However, the climatic interpretation of a key proxy, the stable water oxygen isotopic ratio in ice cores (δ(18)O(ice)), remains an outstanding problem. Here, combining...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10631737/ https://www.ncbi.nlm.nih.gov/pubmed/37939192 http://dx.doi.org/10.1126/sciadv.adi6725 |