Temperature and precipitation effects on the isotopic composition of global precipitation reveal long-term climate dynamics
Abstract Earth’s climate history is traced through the long-term covariance between the isotopic (δ 18O) 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 18O, T an...
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| Autores principales: | , , |
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| Formato: | article |
| Lenguaje: | EN |
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Nature Portfolio
2021
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| Acceso en línea: | https://doaj.org/article/372990428b05408c91950fee0d86a6bb |
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