中国农业气象 ›› 2026, Vol. 47 ›› Issue (5): 769-780.doi: 10.3969/j.issn.1000-6362.2026.05.011

• 农业气象灾害栏目 • 上一篇    下一篇

1981−2024年青海省东部地区冰雹的时空分布特征

康晓燕,王启花,田建兵,薛丽梅,郭世钰   

  1. 1. 青海省气象灾害防御技术中心,西宁 810001;2. 青海省人工影响天气中心,西宁 810001
  • 收稿日期:2025-04-07 出版日期:2026-05-20 发布日期:2026-05-18
  • 作者简介:康晓燕,E-mail:kxy3155@163.com
  • 基金资助:
    青海省科技厅应用基础研究项目(2023-ZJ-727);青海省气象局重点项目(QXZD2025-07)

Spatiotemporal Distribution Characteristics of Hail in Eastern Qinghai Province from 1980 to 2024

KANG Xiao-yan, WANG Qi-hua, TIAN Jian-bing, XUE Li-mei, GUO Shi-yu   

  1. 1.Qinghai Meteorological Disaster Prevention Technology Center, Xi’ning 810001, China; 2.Qinghai Weather Modification Center, Xi’ning 810001
  • Received:2025-04-07 Online:2026-05-20 Published:2026-05-18

摘要:

基于19812024年青海省东部地区冰雹观测资料,运用MannKendall检验和小波分析等方法,分析冰雹发生次数、大小和持续时间的时空变化特征,以期了解该地区冰雹发生、发展和异常变化规律,为区域防雹减灾、保障农业生产安全提供依据。结果表明:(119812024年青海省东部地区年平均降雹次数为35.5次,冰雹平均直径为6.2mm,平均单次降雹持续时间为6.9min。(219812024年青海省东部地区降雹次数以1.08·a−1的速率极显著减少(P0.001),冰雹直径和降雹持续时间无显著变化,降雹次数、直径和降雹持续时间均在7月达峰值。从日尺度看,降雹事件主要发生在午后至傍晚(1400−1700),冰雹直径和降雹持续时间的日峰值出现在2100左右。降雹次数、冰雹直径及降雹持续时间分别于2001年、1994年、1984年存在明显的突变,且存在23a5a56a的周期振荡。(319812024年降雹次数的空间格局与年代际降雹次数分布一致,均表现为西北多、东南少的空间特征,且降雹次数与海拔呈显著正相关关系。综上,19812024年青海省东部地区冰雹活动呈减少趋势,对当地农业生产较为有利,但该区域气候系统复杂,仍需关注局部地区强降雹事件的发生。

关键词: 青海省东部地区, 冰雹, 变化趋势, 气候突变, 周期变化

Abstract:

 Based on hail observation data from eastern Qinghai province between 1981 and 2024, this study investigated spatiotemporal variations in the frequency, diameter and duration of hail events using methods such as MannKendall test and wavelet analysis. The aim was to understand the formation, development and anomaly patterns of hail in this region, thereby providing a basis for hail suppression, disaster mitigation and the safeguarding of agricultural production. The results showed that: (1) the mean annual number of hail events in eastern Qinghai province from 1981 to 2024 was 35.5. The average diameter of hail was 6.2mm, and the average duration per event was 6.9min. (2) During the study period, the annual hail frequency decreased significantly at a rate of 1.08 events per year, while the hail diameter and duration exhibited no significant trends. Hail occurrence displayed strong seasonality, with frequency, diameter and duration all peaking in July. On a diurnal scale, hail events primarily occurred in the afternoon (14:00 to 17:00), whereas the maximum hail diameter and duration were observed at 21:00. The frequency of hail events, hail diameter and duration exhibited abrupt changes in 2001, 1994 and 1984 respectively, showing periodic oscillations of 2−3 years, 5 years and 5−6 years. (3) The spatial pattern of hail frequency from 1981 to 2024 was consistent with the interdecadal distribution, both exhibiting more occurrences in the northwest and less occurrences in the southeast. Additionally, hail frequency demonstrated a significant positive correlation with altitude. In conclusion, hail activity in eastern Qinghai has shown a decreasing trend over the past 44 years, which is relatively favorable for local agricultural production. However, due to the complexity of the regional climate system, attention should still be paid to localized severe hail events.

Key words: Eastern region of Qinghai province, Hail, Change trend, Climate mutation, Periodic change