June 30, 2016 report
Study of stalagmites in caves in China reveals 640,000 years of Asian monsoon history
The annual monsoon season in Asia is a major event, bringing rains that are used to grow crops for an enormous number of people. Because of its importance, scientists would like to know more about it, such as what might happen as the planet heats up. To learn more, the researchers looked for a way to look back at what has happened in the past, and to do that, they ventured to the mountains in central China and descended into Sanbao Cave—there stalagmites have been growing up from the cave floor for hundreds of thousands of years, carrying with them, a history of the factors that led to their growth.
The stalagmites grow at different rates depending on how much rain falls and leaks through the mountain above and down into the cave—during heavy rains, such as occur during monsoon seasons, layers of calcium carbonate build up, holding information about the air and rainwater at a particular point in time, which scientists can analyze to gain a good measurement of climate conditions. They can also look for dissolved uranium, which can be used to date the layers of stalagmite buildup. Together, the two sources of information can be used to create a climate timetable for past monsoon seasons, going back as far as 640,000 years—the most detailed and accurate monsoon record to date. In so doing, the researchers were also able to show that changes in solar radiation over the Northern Hemisphere were due to the planet's precession cycle (a shift that occurs periodically in the planet's axis of rotation)—which wound up bringing an end to the past seven ice ages.
Oxygen isotope records from Chinese caves characterize changes in both the Asian monsoon and global climate. Here, using our new speleothem data, we extend the Chinese record to cover the full uranium/thorium dating range, that is, the past 640,000 years. The record's length and temporal precision allow us to test the idea that insolation changes caused by the Earth's precession drove the terminations of each of the last seven ice ages as well as the millennia-long intervals of reduced monsoon rainfall associated with each of the terminations. On the basis of our record's timing, the terminations are separated by four or five precession cycles, supporting the idea that the '100,000-year' ice age cycle is an average of discrete numbers of precession cycles. Furthermore, the suborbital component of monsoon rainfall variability exhibits power in both the precession and obliquity bands, and is nearly in anti-phase with summer boreal insolation. These observations indicate that insolation, in part, sets the pace of the occurrence of millennial-scale events, including those associated with terminations and 'unfinished terminations'.
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