Abstract
Studying the mechanisms by which climate change interacted with human societies during the historical period can provide historical insights and cultural roots for climate policy building in the region. In this study, we constructed Stability-Robustness-Resilience Model (SSR model) and used the TOPSIS method (Technique for Order Preference by Similarity to Ideal Solution) and the entropy weight method to assess the change processes of robustness, resilience, and stability of Ming's society in response to climate threats. We have also compared three extreme droughts that occurred in different periods of social robustness-resilience combinations by using the SRR model. The results are as follows. (1) The stability of the Ming society was high in YongLe - HongZhi period (1402-1505 CE), when both social robustness and resilience were higher than the average level of Ming Dynasty (0.5611 for the former and 0.4215 for the latter), but there was a significant decline in social stability in TianShun period (1457-1464 CE). In ZhengDe - ChongZhen period (1506-1644 CE), the stability of Ming society gradually decreased, and it rebounded shortly in the LongQing-WanLi period (1506-1620 CE). (2) The high stability benefited from higher socio-economic levels, better government finance levels, larger national food reserves, safer social environments (high robustness), and higher levels of ruling class governance and risk response (high resilience); whereas insecure social environment induced by war, declining socio-economic levels and government finance levels were the main reasons for the decline in society's stability. (3)The ChengHua and WanLi droughts both happened at a time with high social robustness, so although their meteorological anomalies were severe, their impact on society was small. While the JiaJing drought happened at a time with low social robustness and resilience, so although the meteorological anomaly was relatively weak, it resulted in a more severe social consequence than the other two events.