18～19世纪气候转冷如何加速清朝衰落
发布时间：2018-08-31 09:34
【摘要】：正18～19世纪之交是清代社会结束所谓"康乾盛世"、进入长达一个世纪的衰落期的转折点。为什么中国社会在此时由盛转衰、由治转乱?除了政治、历史等因素之外,气候变化这个不曾被广泛关注的因素或许也为加速清朝衰落"贡献"了力量。最近由北京师范大学地理学与遥感科学学院方修琦教授及中国科学院地理科学与资源研究所萧凌波博士等人合作完成的一项研究结果显示,以急速降温和极端旱涝灾害频次增加为标志的气候变
[Abstract]:At the turn of the 19th century, it was the turning point for the Qing Dynasty to end the so-called "Kangqian prosperous period" and enter a century-long period of decline. Why did Chinese society change from prosperity to decline and from governance to chaos at this time? Apart from political, historical and other factors, climate change, which has not received much attention, may have contributed to accelerating the decline of the Qing Dynasty. A recent study by Professor Fang Xiuqi, School of Geography and remote Sensing Sciences, Beijing normal University, and Dr. Xiao Lingbo, Institute of Geography and Resources, Chinese Academy of Sciences, shows that Climate change marked by rapid cooling and increasing frequency of extreme drought and waterlogging disasters
【分类号】：K249;P467
，
本文编号：2214592
[Abstract]:At the turn of the 19th century, it was the turning point for the Qing Dynasty to end the so-called "Kangqian prosperous period" and enter a century-long period of decline. Why did Chinese society change from prosperity to decline and from governance to chaos at this time? Apart from political, historical and other factors, climate change, which has not received much attention, may have contributed to accelerating the decline of the Qing Dynasty. A recent study by Professor Fang Xiuqi, School of Geography and remote Sensing Sciences, Beijing normal University, and Dr. Xiao Lingbo, Institute of Geography and Resources, Chinese Academy of Sciences, shows that Climate change marked by rapid cooling and increasing frequency of extreme drought and waterlogging disasters
【分类号】：K249;P467
，
本文编号：2214592
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