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Global warming will shift the East Asian monsoon rain belt northward
Author: | Update time:2015-10-21           | Print | Close | Text Size: A A A

The East Asian monsoon has been decreasing since 1970s. As a result, the monsoon rain belt has migrated southward, with more droughts in northern China countered by more floods in southern China. The trend of decreasing monsoon intensity has been attributed to global warming by many scientists, thus raising great concerns over further drying in northern China as global warming continues. It is crucial to identify whether the recent drying is transient or if it signals the start of a long-term drying trend induced by global warming.  

Glacial–interglacial changes in the distribution of C3/C4 vegetation on the Chinese Loess Plateau have been related to East Asian summer monsoon intensity and position, and could provide insights into future changes caused by global warming. For the past several years, Shiling Yang, Zhongli Ding and colleagues from IGGCAS have investigated over 20 loess-soil sections. By measuring 14C ages and carbon isotope compositions (d13C) of soil organic matter, they reconstructed the spatiotemporal pattern of C4 vegetation on the Chinese Loess Plateau for the past 20 ka. The results show that C4 vegetation increased gradually both from the LGM to the mid-Holocene in each section and from northwest to southeast in each time interval (Fig. 1), indicating that C4 biomass is closely related to the summer monsoon precipitation.  

Further analysis shows that the isolines of C4 biomass exhibit a northeast–southwest zonal distribution pattern, closely resembling the pattern of present monsoon precipitation (Fig. 1). Thus the migration of C4 isolines effectively indicates a change in the position of the monsoon rain belt. The 10–20% isolines for C4 biomass in the southeastern part of the Loess Plateau during the LGM moved to the northwestern part during the mid-Holocene, indicating a northwesterly monsoon rain belt advance of 300 km for the warm Holocene compared with the cold LGM (Fig. 2). These results show that global warming will shift the East Asian monsoon rain belt northwestward. It follows that the southward displacement of the monsoon rain belt and the drying trend observed during the last few decades in northern China will reverse as global warming continues. The findings provide a scientific basis for the evaluation of the effect of global warming on the climate and the ecologically vulnerable areas in northern China. 

This study was recently published in PNAS (Yang et al., Warming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-Holocene, PNAS, 2015.). 

Fig. 1. Contour maps of estimated C4 biomass (%) for the Last Glacial Maximum (LGM) and the mid-Holocene, together with modern mean warm-season precipitation (May to September) over 51 y (1951–2001). Note the migration of the 10–20% isolines for C4 biomass (pink lines) between the LGM and the mid-Holocene.  

Fig. 2. Migration of the East Asian summer monsoon rain belt (purple dashed lines) between the Last Glacial Maximum (LGM) and the mid-Holocene as reconstructed using the 10–20% isolines for C4 biomass shown in Fig. 1. The monsoon rain belt migrated at least 300 km to the northwest from the cold Last Glacial Maximum (19 ka) to the warm Holocene (4 ka). 


YANG Shiling 
Division of Cenozoic Geology and Environment, IGGCAS 

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