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. 2023 May 25;2(6):pgad175. doi: 10.1093/pnasnexus/pgad175

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© The Author(s) 2023. Published by Oxford University Press on behalf of National Academy of Sciences.

This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.

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Fig. 4. — Comparison of Asian monsoon anomaly records with the global ice volume and the NHSI. Aridity anomaly (Δ Fe/norm sum.) and winter wind anomaly [Δ ln (Fe/Si) norm.] in the Indian–Asian landmass in comparison with anomaly in the EASM (12) (Δ δ18O norm.). The increase in arid anomaly conditions occurred in both the EASM and the Indian–Asian landmass during the increase in insolation. Note that the main aridity anomaly events occurred concurrently with the major drops in the values of LR04 during sea-level rise.