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Temperature and precipitation effects on the isotopic composition of global precipitation reveal long-term climate dynamics
Earth’s climate history is traced through the long-term covariance between the isotopic (δ (18)O) composition of archived meteoric waters (groundwater, ice cores) with air temperature (T) and amount of precipitation (P). To assess recent multi-decadal climatic changes, we analysed δ(18)O, T and P, a...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8445972/ https://www.ncbi.nlm.nih.gov/pubmed/34531502 http://dx.doi.org/10.1038/s41598-021-98094-6 |