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Changes in the amount of summer incoming solar radiation (insolation) reaching the Northern Hemisphere are the underlying pacemaker of glacial cycles1, 2, 3, 4, 5, 6. However, not all rises in boreal summer insolation over the past 800,000 years resulted in deglaciation to present-day ice volumes1, 2, 3, 6, 7, 8, suggesting that there may be a climatic threshold for the disappearance of land-based ice.
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