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Paleogeographic modulation of Phanerozoic climate by albedo compensation of interhemispheric land imbalances
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DOI：10.1016/j.earscirev.2026.105632.png)
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Abstract
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• Compiled 53 paleogeographic reconstructions from 530 Ma to present. • Land and sea distributions estimated in four zonal climate belts per hemisphere. • Interhemispheric surface reflectivity imbalances require compensation. • Compensated surface reflectivity modulates absorbed solar flux and glacial preconditions. • Surface reflectivity variations rival CO₂ forcing in shaping long-term climate.
Keywords:
Phanerozoic
Paleogeography
Surface reflectivity
Cloud compensation
Absorbed solar flux
Ice ages
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