Distinctive changes of Asian–African summer monsoon in interglacial epochs and global warming scenario
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00382-023-07013-0.pdf
Reference109 articles.
1. Bartlein PJ et al (2011) Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Clim Dyn 37:775–802. https://doi.org/10.1007/s00382-010-0904-1
2. Berger A, Loutre MF (1991) Insolation values for the climate of the last 10 million years. Quat Sci Rev 10:297–317. https://doi.org/10.1016/0277-3791(91)90033-Q
3. Biasutti M (2013) Forced Sahel rainfall trends in the CMIP5 archive. J Geophys Res Atmos 118:1613–1623. https://doi.org/10.1002/jgrd.50206
4. Bony S, Bellon G, Klocke D, Sherwood S, Fermepin S, Denvil S (2013) Robust direct effect of carbon dioxide on tropical circulation and regional precipitation. Nat Geosci 6:447–451. https://doi.org/10.1038/ngeo1799
5. Boos WR, Korty RL (2016) Regional energy budget control of the intertropical convergence zone and application to mid-Holocene rainfall. Nat Geosci 9:892–897. https://doi.org/10.1038/ngeo2833
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