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Ice core δ 18 O evidence for climatic transition since 1990s on East Rongbuk Glacier
Abstract Ice core stable water isotope (δ18O) records serve as reliable proxies for temperature on long timescales in both polar and tropical high-elevation regions. However, the climatic implications of ice core δ18O over the monsoon-influenced southern Tibetan Plateau remain poorly understood. Here, we establish the East Rongbuk (ERB) ice core chronology spanning 1952–2021 for the central Himalaya through cross-dating of δ18O records from five ERB ice cores.
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