氣候變化研究進(jìn)展 ?? 2024, Vol. 20 ?? Issue (2): 146-157.doi: 10.12006/j.issn.1673-1719.2023.219
收稿日期:
2023-10-07
修回日期:
2023-11-27
出版日期:
2024-03-30
發(fā)布日期:
2024-03-11
通訊作者:
楊煜達(dá),男,研究員,ydyang@fudan.edu.cn
作者簡(jiǎn)介:
劉威,女,博士研究生,基金資助:
LIU Wei(), YANG Yu-Da(), ZHANG Sen
Received:
2023-10-07
Revised:
2023-11-27
Online:
2024-03-30
Published:
2024-03-11
摘要:
以歷史文獻(xiàn)為主要代用資料,重建了1632年華北地區(qū)暴雨洪澇事件的雨情、水情、災(zāi)情等,從而識(shí)別出1632年8月河南地區(qū)暴雨事件的時(shí)空范圍,并與有器測(cè)記錄的2021年河南極端降水事件進(jìn)行對(duì)比。1632年華北地區(qū)大規(guī)模降水始于7月17日,從6月18日—11月11日,整個(gè)華北不同區(qū)域皆存有長時(shí)間降雨記錄,且有多次強(qiáng)降水記錄,造成黃淮地區(qū)雨澇,并使得黃淮交潰,對(duì)社會(huì)經(jīng)濟(jì)造成較大影響。梳理降水和洪澇的過程,區(qū)分了本地降水與客水的分布。將1632年8月河南暴雨洪澇與2021年7月河南極端降水事件對(duì)比發(fā)現(xiàn),強(qiáng)降水位置相似,降水前后都有兩個(gè)臺(tái)風(fēng)輸送水汽,且1632和2021年華北地區(qū)夏季降水皆受到拉尼娜的影響,整體偏澇。
劉威, 楊煜達(dá), 張森. 1632年華北地區(qū)暴雨洪澇事件研究[J]. 氣候變化研究進(jìn)展, 2024, 20(2): 146-157.
LIU Wei, YANG Yu-Da, ZHANG Sen. Reconstruction of the 1632 rainstorm and flooding event in North China[J]. Climate Change Research, 2024, 20(2): 146-157.
圖6 2021年7月(a)與1632年8月(b)河南極端降水對(duì)比 注:(a)圖為2021年7月19日08時(shí)—22日08時(shí)降水量[28],(b)圖為1632年8月3—7日降水分布。
Fig. 6 Comparison of extreme precipitation events in Henan province between July 2021 (a) and August 1632 (b)
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