Stalagmite-inferred variability of the Asian summer monsoon during the penultimate glacial–interglacial period

The orbital-timescale dynamics of the Quaternary Asian summer monsoons (ASM) are frequently attributed to precession-dominated northern hemispheric summer insolation. However, this long-term continuous ASM variability is inferred primarily from oxygen isotope records of stalagmites, mainly from Sanb...

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Bibliographic Details

Published in:	Climate of the Past
Main Authors:	T.-Y. Li, C.-C. Shen, L.-J. Huang, X.-Y. Jiang, X.-L. Yang, H.-S. Mii, S.-Y. Lee, L. Lo
Format:	Article
Language:	English
Published:	Copernicus Publications 2014-06-01
Online Access:	http://www.clim-past.net/10/1211/2014/cp-10-1211-2014.pdf