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汤兴芝, 黄治勇, 张荣, 王文玉, 姚瑶. 2023: 2010—2020年全国冰雹灾害事件时空分布特征. 暴雨灾害, 42(2): 223-231. DOI: 10.12406/byzh.2022-089
引用本文: 汤兴芝, 黄治勇, 张荣, 王文玉, 姚瑶. 2023: 2010—2020年全国冰雹灾害事件时空分布特征. 暴雨灾害, 42(2): 223-231. DOI: 10.12406/byzh.2022-089
TANG Xingzhi, HUANG zhiyong, Zhang Rong, WANG Wenyu, YAO yao. 2023: Temporal and spatial distribution characteristics of hail disaster events in China from 2010 to 2020. Torrential Rain and Disasters, 42(2): 223-231. DOI: 10.12406/byzh.2022-089
Citation: TANG Xingzhi, HUANG zhiyong, Zhang Rong, WANG Wenyu, YAO yao. 2023: Temporal and spatial distribution characteristics of hail disaster events in China from 2010 to 2020. Torrential Rain and Disasters, 42(2): 223-231. DOI: 10.12406/byzh.2022-089

2010—2020年全国冰雹灾害事件时空分布特征

Temporal and spatial distribution characteristics of hail disaster events in China from 2010 to 2020

  • 摘要: 基于中国气象局气象灾害管理系统冰雹灾情数据,运用统计方法和GIS技术,对2010—2020年中国冰雹灾害事件时空分布特征进行研究,结果表明: (1) 2010—2020年,全国冰雹事件出现的站数和站日数在增加,大冰雹事件则相反呈减少趋势。(2) 冰雹季节性明显,夏季和冬季分别为冰雹站日数最多和最少的季节,6月最多,11月最少,西南和华中地区表现为双峰结构,其他为单峰结构;大冰雹月变化与冰雹类似,但12月最少,且在西南地区表现为单峰结构。(3)日变化上,冰雹/大冰雹主要集中于午后至傍晚。华南呈现双峰结构,其他地区呈单峰结构,西北地区峰值出现时间比其他地区晚1 h。(4) 空间分布上,西北、西南和华北地区的冰雹/大冰雹站日数明显高于其它地区,而东北、华南大冰雹站日数比例高于其他地区。冰雹/大冰雹年均日数呈带状多区分布,最多的为云贵高原,其次为秦岭、阴山、大兴安岭及天山一带。而低发区的华东地区在春季反而成为大冰雹的高发区。(5) 海拔高度分布上,在1.5—2 km处最易出现冰雹,在1— 1.5 km高度上最易出现大冰雹;冬季冰雹主要在海拔高度2 km以下,随着温度升高,高海拔冰雹逐渐增多,9月高海拔地区冰雹比例达到最大。

     

    Abstract: Based on the hail data of the China Meteorological Administration, the spatial and temporal distributions of hail disaster eents in China during 2010-2020 are studied by using the statistical method and GIS technology. The result is shown below. (1) The number of stations and the days of hails in China increase, while the number of severe hails decreases during 2010-2020. (2) The seasonal change is significant for the number of stations and the days of hails with the maximum in summer and the minimum in winter. In terms of monthly variation, hail occurs most often in June and least often in November. In southwest and central China, the monthly variation of the number of stations and the days of hails is bimodal. The monthly distribution of severe hail is similar to that of hail, but it occurs least often in December. The severe hail occurs most frequently in southwest China. (3) For diurnal variation, hail or severe hail mainly occurrs from afternoon to evening. The peak appears 1-hour later in northwest China than in other areas. (4) In terms of spatial distribution, the number of stations and the days of hail or severe disaster in Northwest, Southwest, and North China are significantly higher than those in the other regions, and the proportion of severe hail in Northeast and South China is higher than that in the other regions. The annual average days of hail or severe hail are distributed in multi-zone bands, and the multi-hail area extends along the mountains, with the largest value located in the Yunnan-Guizhou Plateau, followed by the mountains of Qinling, Yinshan, Daxing 'anling, and Tianshan. In addition, the low-incidence area of eastern China in spring has become a high-incidence area of hail. (5)From the elevation distribution, hail is most likely to occur at the altitude of 1.5-2 km, and severe hail is most likely to occur at the altitude of 1-1.5 km. In winter, hail is mainly below 2 km. With the rise of temperature, hail gradually increases in the high-altitude areas, and the proportion of hailstones in the high-altitude areas reaches the maximum in September.

     

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