Abstract
Before the end of the Ming Dynasty to the early of the Qing Dynasty, climate was warm, and heat energy was plentiful, so double-cropping of rice in Taihu Lake basin could grow without any protection. Later the global climate entered the Little Ice Age, the double-cropping of rice was extirpated nearly, grain output decreased heavily. After the Little Ice Age, although, the global climate got warm, sometimes, the thermal condition was enough for two crops no three crops one year throughout the period. So both the area and output of of double-cropping of rice was fluctuated with variation of cold/ warm. The condition of heat energy, with the movement of climatic zone, becomes a sensitive factor effecting grain production. Recently, as CO2concentration in atmosphere is increasing, climate is getting warm. With the comprehensive effect of such warming and natural cooling trend, the climate in Taihu Lake basin shows the following trend: warm in winter, cooling in summer, decreasing of annual accumulated temperature and advancing of autumn low temperature. This trend will strongly influence the grain production.
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References
佘 之祥. 太湖地区的农业与农村发展问题—太 湖流域水土资源及农业发展远景研究. 见: 中国科学院南京地理与湖研究所集刊专辑, 北京: 科学出版社, 1988.
陈家其. 从太湖流域历史旱;史料看历史 气候信息处理. 地理学报, 1987, 42 (3).
朱瑞熙. 宋代 “苏湖;, 天下足” 语的形成. 农业考古, 1987, 48–49.
陈志一. 江苏双季稻和历史初探. 中国农史, 1983. 22–23.
闵宗殿. 宋明清时期太湖地区水稻;产量的探讨. 中国农史, 1984. 37–42.
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Shen, X., Chen, J. Grain production and climatic variation in taihu lake basin. Chinese Geographical Science 3, 173–178 (1993). https://doi.org/10.1007/BF02664558
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DOI: https://doi.org/10.1007/BF02664558