公元1600年秘鲁Huaynaputina火山喷发在中国的气候效应  

The Possible Climatic Impact of the A.D.1600 Huaynaputina Eruption,Peru to China

作　　者：费杰[1] 

机构地区：[1]中国科学技术大学科技史与科技考古系

出　　处：《灾害学》2008年第2期65-70,共6页Journal of Catastrophology

基　　金：中国博士后基金(20060400732);中国科学院知识创新工程方向性项目(KZCX3-SW-146);2006年度中国科学院院长奖获得者科研启动专项资金

摘　　要：公元1600年秘鲁Huaynaputina火山喷发是历史时期全球最大规模的火山喷发之一,在全球范围产生了重大的气候与环境效应。通过对中国历史时期地方志文献的查阅与整理,结合南北极的冰芯、北半球的树轮和欧洲历史文献等有关记录,对Huaynaputina火山喷发在中国的气候效应进行探讨。结果发现1601年夏季长江下游地区异常寒冷,1601年夏季和秋季黄河中下游地区的严重霜灾,1602年上半年长江中下游地区异常多雪。The Huaynaputina eruption in A. D. 1600 is one of the greatest historical volcanic＇eruptions in the world in the historical times. Evidences of the potential environmental and climatic impacts of the eruption are found in ice cores, tree ring chronologies and European historical literatures. The possible climatic impact of the eruption to China is investigated by consulting the Chinese historical local chronicles. The results show that it was unusual cold in the summer of A. D. 1601 in the lower reaches of the Yangtze River, severe frost disasters occurred in the summer and autumn of A.D. 1601 in the middle and lower reaches of the Yellow River and there was unusual heavy snowfall in early A.D. 1602 in the middle and lower reaches of the Yangtze River.

关 键 词：Huaynaputina 火山喷发 气候效应 冰芯 树轮 地方志 秘鲁 中国 

分 类 号：X43[环境科学与工程—灾害防治]