Regional synthesis of Mediterranean atmospheric circulation during the Last Glacial Maximum
Atmospheric circulation leaves few direct traces in the geological record, making reconstructions of this crucial element of the climate system inherently difficult. We produced a regional Mediterranean synthesis of paleo-proxy data from the sea surface to alpine altitudes. This provides a detailed observational context for change in the three-dimensional structure of atmospheric circulation between the Last Glacial Maximum (LGM, ∼23,000 to 19,000 years ago) and the present. The synthesis...[Show more]
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