The Holocene Asian monsoon: links to solar changes and North Atlantic climate
- PMID:15879216
- DOI: 10.1126/science.1106296
The Holocene Asian monsoon: links to solar changes and North Atlantic climate
Abstract
A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years. Although the record broadly follows summer insolation, it is punctuated by eight weak monsoon events lasting approximately 1 to 5 centuries. One correlates with the "8200-year" event, another with the collapse of the Chinese Neolithic culture, and most with North Atlantic ice-rafting events. Cross-correlation of the decadal- to centennial-scale monsoon record with the atmospheric carbon-14 record shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.
Comment in
- Atmospheric science. Changes in the sun may sway the tropical monsoon.Kerr RA.Kerr RA.Science. 2005 May 6;308(5723):787. doi: 10.1126/science.308.5723.787.Science. 2005.PMID:15879189No abstract available.
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