Articles | Volume 10, issue 5
Clim. Past, 10, 1803–1816, 2014

Special issue: Western Pacific paleoceanography – an ocean history...

Clim. Past, 10, 1803–1816, 2014

Research article 01 Oct 2014

Research article | 01 Oct 2014

Variation in the Asian monsoon intensity and dry–wet conditions since the Little Ice Age in central China revealed by an aragonite stalagmite

J.-J. Yin et al.

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Cited articles

Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M. N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G.: Persistent solar influence on North Atlantic climate during the Holocene, Science, 294, 2130–2136, 2001.
Broecker, W. S. and Putnam, A. E.: Hydrologic impacts of past shifts of earth's thermal equator offer insight into those to be produced by fossil fuel CO2, P. Natl. Acad. Sci., 110, 16710–16715, 2013.
Burns, S. J., Fleitmann, D., Mudelsee, M., Neff, U., Matter, A., and Mangini, A.: A 780-year annually resolved record of Indian Ocean monsoon precipitation from a speleothem from south Oman, J. Geophys. Res., 107, 4434,, 2002.
Cai, Y., Tan, L., Cheng, H., An, Z., Edwards, R. L., Kelly, M. J., Kong, X., and Wang, X.: The variation of summer monsoon precipitation in central China since the last deglaciation, Earth Planet. Sc. Lett., 291, 21–31, 2010.