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Reconstructing the extent, style, timing and drivers of past mountain glaciation is crucial in both understanding past atmospheric circulation and predicting future climate change. Unlike in high-elevation mountains situated in maritime and continent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::502c49d16a9fd2a4e901e92be23e9f0b
https://doi.org/10.5194/egusphere-egu22-2910
https://doi.org/10.5194/egusphere-egu22-2910
