Earth Surface Processes

The influence of historical climate change on agriculture in ancient China

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  • Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China

Received date: 2010-07-03

  Revised date: 2010-10-26

  Online published: 2010-12-20

Abstract

This paper made an analysis of the relationship between climate change and agricultural development in China since the Qin Dynasty. The following conclusions are obtained about how historical climate fluctuation influenced ancient agricultural production. Warm periods were beneficial to agricultural development while cold periods made against to it. When the climate was warm (e.g. Qin, Han, Sui and Tang dynasties), the northern boundary of farming moved northward. Thus, cultivation area expanded. And crop growing time and cropping patterns would also increase due to relatively high temperature. As a result, crop yields were greatly improved. However, during cold periods, (e.g. Wei, Jin, Northern and Southern Dynasties, Late Tang Dynasty and Five Dynasties period), the boundary of farming moved southward, cropping patterns became single, cultivation land and crop growing time reduced. These changes caused the decrease of crop yield. Moreover, the history of rice distribution in ancient China shows that during warm periods, single cropping rice was widely planted in the Yellow River Basin, and double cropping rice could grow in the Yangtze River Basin. But when the climate became cold, the range of the distribution of single cropping rice plant in the Yellow River Basin was significantly diminished, and double cropping rice retreated to the south of the Yangtze River Basin.

Cite this article

HE Fan-neng, LI Ke, LIU Hao-long . The influence of historical climate change on agriculture in ancient China[J]. GEOGRAPHICAL RESEARCH, 2010 , 29(12) : 2289 -2297 . DOI: 10.11821/yj2010120018

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