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黄河旱涝变化特征及应对过程

靖娟 赵鑫 梅瑞萱 尚文绣

人民黄河2024,Vol.46Issue(7):22-28,7.
人民黄河2024,Vol.46Issue(7):22-28,7.DOI:10.3969/j.issn.1000-1379.2024.07.004

黄河旱涝变化特征及应对过程

Characteristics of Drought and Wetness in the Yellow River and Its Countermeasures

靖娟 1赵鑫 1梅瑞萱 2尚文绣1

作者信息

  • 1. 黄河勘测规划设计研究院有限公司,河南 郑州 450003
  • 2. 中国人民大学 农业与农村发展学院,北京 100089
  • 折叠

摘要

Abstract

In order to scientifically identify the characteristics of drought and wetness in the Yellow River and the coping capacity,this paper put forward a judgment method of continuous wet years and continuous dry years,used the Standardized Runoff Index(SRI)and the Stand-ardized Drought-Wetness Abrupt Alteration Index(SDWAI)to identify the characteristics of runoff changes at Lijin Station of the Yellow Riv-er from 1956 to 2020,and analyzed the role of reservoir operation in coping with the drought-wetness abrupt alteration events and continuous dry years.The results show that on a monthly scale,the SRI assessment results of Lijin Station are mainly normal to moderate drought,with only a few drought-wetness abrupt alteration events which mainly happen during the transition period between flood season and non-flood sea-son.On an annual scale,more than 60%of the years are assessed as normal or light drought,and the SRI assessment results are consistent with the assessment results using anomaly value.On a multi-year scale,there are 3 continuous wet years and 2 continuous dry years at Lijin Station,and the continuous dry years last for a long time.With the enhancement of reservoir regulation and storage capacity,drought-wetness abrupt alteration events are handled well,but the capacity to cope with continuous dry years is insufficient.

关键词

旱涝急转/连续丰水年/连续枯水年/判定方法/水库调度/黄河

Key words

drought-wetness abrupt alteration/continuous wet years/continuous dry years/judgment method/reservoir operation/Yellow River

分类

建筑与水利

引用本文复制引用

靖娟,赵鑫,梅瑞萱,尚文绣..黄河旱涝变化特征及应对过程[J].人民黄河,2024,46(7):22-28,7.

基金项目

国家重点研发计划项目(2022YFC3202300) (2022YFC3202300)

河南省重大科技专项(201300311400) (201300311400)

人民黄河

OA北大核心CSTPCD

1000-1379

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