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Hu, C.,Henderson, G.M.,Huang, J.,Xie, S.,Sun, Y.,Johnson, K.R. 2008 Quantification of Holocene Asian monsoon rainfall from
spatially separated cave records. Earth and Planetary Science Letters Vol. 266, pp. 221-232, Issues 3-4
| Data Coverage |
North: 30.45 * South: 30.45 |
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West: 110.416 * East: 110.416 |
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Altitude: 294 m |
Start Year: -7470 AD
End Year: 2000 AD
Data: Please Cite Data Contributors!
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Summary: A reconstruction of Holocene rainfall is presented for southwest China -
an area prone to drought and flooding due to variability in the East
Asian monsoon. The reconstruction is derived by comparing a new high-
resolution stalagmite d18O record with an existing record from the same
moisture transport pathway. The new record is from Heshang Cave
(30°27'N, 110°25'E; 294 m) and shows no sign of kinetic or evaporative
effects so can be reliably interpreted as a record of local rainfall
composition and temperature. Heshang lies 600 km downwind from Dongge
Cave which has a published high-resolution d18O record (Wang, Y.J.,
Cheng, H., Edwards, R.L., He, Y.Q., Kong, X.G., An, Z.S., Wu, J.Y.,
Kelly, M.J., Dykoski, C.A., Li, X.D., 2005. The Holocene Asian monsoon:
links to solar changes and North Atlantic climate. Science 308, 854¿857).
By differencing co-eval d18O values for the two caves, secondary controls
on d18O (e.g. moisture source, moisture transport, non-local rainfall,
temperature) are circumvented and the resulting Dd18O signal is
controlled directly by the amount of rain falling between the two sites.
This is confirmed by comparison with rainfall data from the instrumental
record, which also allows a calibration of the Dd18O proxy. The calibrated
Dd18O record provides a quantitative history of rainfall in southwest
China which demonstrates that rainfall was 8% higher than today during
the Holocene climatic optimum (~6 ka), but only 3% higher during the
early Holocene. Significant multi-centennial variability also occurred,
with notable dry periods at 8.2 ka, 4.8¿4.1 ka, 3.7¿3.1 ka, 1.4¿1.0 ka
and during the Little Ice Age. This Holocene rainfall record provides
a good target with which to test climate models. The approach used here,
of combining stalagmite records from more than one location, will also
allow quantification of rainfall patterns for past times in other regions.
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