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SUMMARY
| https://doi.org/10.1038/s41467-022-28939-9 D etermining the impact of past climate variability on centennial to millennial-scale glacier fluctuations during the Holocene is critical to better understand the respective influence of natural and anthropogenic contributions to current and future glacier retreat1. Consistent with this summer insolation trend, it is generally considered that Northern Hemisphere mid-latitude glaciers increased in extent throughout the mid and late Holocene, recording their maximum size during the Little Ice Age (LIA), while most Southern Hemisphere glaciers gradually retreated until a minimum ice extent was . . .
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