Climatic influences on stable water isotope variability in palaeo-precipitation
Stable water isotopes are useful tracers in the hydrological cycle that preserve integrated histories of water transport. Water isotope archives such as speleothems (calcium carbonate cave deposits) and ice cores provide evidence of past changes in the atmospheric water cycle. Climatic interpretations from past isotopic variability in proxy records often consider changes as an index of a single climate parameter, such as temperature or precipitation amount. The isotopic composition of...[Show more]
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