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Extreme climate events, migration for cultivation and policies: A case study in the early Qing Dynasty of China

机译:极端气候事件,耕种和政策迁移:以中国清朝初期为例

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Based on the historical records of the annual increase in the workforce (men older than 16 years of age), the annual new taxed cropland in the Shengjing area (Northeast China), the extreme climate events in North China, and related management policies in Northeast China during 1661 -1680, a case study has been conducted to investigate the relationship between the extreme climate events in North China and the migration to Northeast China for cultivation. This study has found that the migration to Northeast China for cultivation from 1661 to 1680 was a response to the drought events that occurred in North China. The upsurge of migration, which occurred in 1665—1680, was a response to the drought period during 1664—1680 in North China while the fewer disasters period in Northeast China. There were three migratory peaks during the upsurge of migration, which corresponded to the three drought events. The peaks of migration, however, often lagged behind the drought events about 1 —2 years. The encouraging-migration policy, which was adopted to encourage cultivation in Northeast China, did not produce much migration into the region in the early Qing Dynasty. It did, however, provide a policy background, which ensured more than 10000 migrants per year to Northeast China when North China suffered from drought/flood disasters. As a response to the highest peak of migration induced by the severe droughts in North China during 1664—1667, a prohibiting-migration policy restricted further migration to Northeast China was carried out in 1668. Although the prohibiting-migration policy could not entirely stop the migrants fleeing from famine in North China to Northeast China, the migrants and cultivation were significantly reduced under the policy. The frequent changes of the policy on the years when taxation started after the land was cultivated were also related to climate events. The extreme climate events in North China, migration to Northeast China for cultivation, and the related management policies showed an impact-response chain, which reflected the interaction among extreme climate events, human behavior, and policies.
机译:根据历史记录,即劳动力的年均增长(16岁以上的男性),盛京地区(中国东北)的年度新征税耕地,华北地区的极端气候事件以及东北地区的相关管理政策在1661年-1680年的中国,进行了一个案例研究,以调查华北极端气候事件与向东北迁移以进行耕种之间的关系。这项研究发现,从1661年到1680年向东北迁移以进行耕种是对华北干旱事件的响应。移民热潮发生于1665年至1680年,是对华北1664年至1680年干旱时期的回应,而东北地区的灾情较少。在迁徙高潮期间有三个迁徙高峰,与三个干旱事件相对应。但是,迁徙的高峰通常落后于干旱事件约1-2年。为了鼓励东北地区的耕种而采取的鼓励迁徙政策在清朝初期并未对该地区产生太多的迁徙。但是,它确实提供了政策背景,当华北遭受干旱/洪灾时,每年有10,000多名移民到中国东北。为了应对1664年至1667年间华北严重干旱导致的最高移民高峰,1668年实施了禁止移民政策,限制了进一步向东北地区的移民。尽管禁止移民政策并不能完全阻止华北地区从饥荒中逃亡到东北地区,该政策大大减少了移民和耕种。耕地后开始征税的年份政策的频繁变化也与气候事件有关。华北地区极端气候事件,向东北迁徙进行耕种以及相关的管理政策均表现出影响-反应链,反映了极端气候事件,人类行为和政策之间的相互作用。

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