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陕西秦岭以北地区清代霜雪灾害与寒冷气候事件研究

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运用灾害等级法、数理统计法、小波分析法等对清代陕西秦岭以北地区的霜雪灾害等级、时空分布、周期性及致灾因子进行研究.结果表明:(1)陕西秦岭以北地区清代(1644-1911 年)268 年内共发生霜雪灾害 97 次,1644-1703 年和1864-1911 年为高频期,1704-1783 年和1784-1863 年为较低频期,且存在3 年、7 年、11 年、28 年的准周期.(2)霜雪灾害频次和等级存在季节性特征.霜灾在春秋两季最为频繁,雪灾在冬春季节发生最多,冻灾几乎仅在冬季发生.中度等级灾害多发生于春秋两季,重度等级灾害常发生于秋冬之际.(3)霜雪灾害的强弱与频次在空间上有较好一致性,多集中于陕北黄土高原北部和西北部以及关中盆地东南部.(4)霜雪灾害发生高频期对应气候更为寒冷干燥.冬季风强度是决定霜雪灾害发生的直接因素.(5)小冰期气候在清代最突出的特点是在较暖或炎热月份发生降温达15~20℃的灾难性降温事件,并导致灾难性天气过程.(6)清代陕西秦岭以北地区发生两次极端寒冷气候事件,分别在1662-1692 年和1861-1900 年,后者指示清代气温最低的时期.
Study on Frost and Snow Disasters and Climatic Events during Qing Dynasty in the North of Qinling Mountains in Shaanxi Province
Using disaster level method,mathematical statistics method,wavelet analysis method to study the frost and snow disaster level,spatiotemporal distribution,periodicity,and disaster causing factors in the North of Qinling Mountains in Shaanxi Province during the Qing Dynasty.The results show that:(1)A total of 97 frost and snow disasters occurred in the North of Qinling Mountains in Shaanxi Province during the 268 years of the Qing Dy-nasty,with 1644-1703 and 1864-1911 being the high-frequency periods,1704-1783 and 1784-1863 being the relatively low-frequency periods,and there were quasi cycles of 3 a,7 a,11 a and 28 a.(2)The frequency and lev-el of frost and snow disasters have seasonal characteristics.Frost disasters are most frequent in spring and autumn,snow disasters occur most frequently in winter and spring,and frost disasters are almost exclusively in winter.Moder-ate level disasters often occur in spring and autumn,while severe level disasters often occur during autumn and win-ter.(3)The strength and frequency of frost and snow disasters have good spatial consistency,mainly concentrated in the northwest of the Loess Plateau in northern Shaanxi and the southeast of the Guanzhong Basin.(4)The high-fre-quency period of frost and snow disasters corresponds to a colder and drier climate.The intensity of winter winds is the direct factor determining the occurrence of frost and snow disasters.(5)The most prominent feature of the Little Ice Age climate in the Qing Dynasty was the catastrophic cooling event that occurred in warmer or hotter months,with temperatures dropping by about 15~20℃,leading to catastrophic weather processes.(6)During the Qing Dynasty,two extreme cold weather events occurred in the north of Qinling Mountains in Shaanxi Province,between 1662-1692 and 1861-1900,respectively.The latter indicated the period of the lowest temperature in the Qing Dynasty.

Qing Dynastyfrost and snow disasterspatial-temporal changecold climate eventsNorth of Qinling Mountains in Shaanxi Province

李嘉宁、岳大鹏、赵景波、杨天宇

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陕西师范大学 地理科学与旅游学院,西安 710119

中国科学院 地球环境研究所,西安 710061

中国科学院 黄土与第四纪地质国家重点实验室,西安 710061

清代 霜雪灾害 时空变化 寒冷气候事件 陕西秦岭以北地区

国家自然科学基金重点项目国家重点实验室项目国家重点实验室项目

42130507SKLLQG2106SKLLQG2013

2024

地域研究与开发
河南省科学院 地理研究所

地域研究与开发

CSTPCDCHSSCD北大核心
影响因子:1.698
ISSN:1003-2363
年,卷(期):2024.43(4)