Journal of Arid Meteorology ›› 2022, Vol. 40 ›› Issue (6): 922-932.DOI: 10.11755/j.issn.1006-7639(2022)-06-0922
• Study on rainstorm in arid region • Previous Articles Next Articles
ZHANG Junxia1,2(), HUANG Wubin2(
), YANG Xiumei2, LIU Weicheng2, ZHOU Zihan2, SHA Honge2
Received:
2022-08-24
Revised:
2022-09-28
Online:
2022-12-31
Published:
2023-01-10
Contact:
HUANG Wubin
张君霞1,2(), 黄武斌2(
), 杨秀梅2, 刘维成2, 周子涵2, 沙宏娥2
通讯作者:
黄武斌
作者简介:
张君霞(1990—),女,甘肃白银人,助理工程师,主要从事模式客观订正方法研究.E-mail:18419611389@163.com。
基金资助:
CLC Number:
ZHANG Junxia, HUANG Wubin, YANG Xiumei, LIU Weicheng, ZHOU Zihan, SHA Honge. Analysis on precipitation extremity of a torrential rain event in semi-arid region of eastern Gansu[J]. Journal of Arid Meteorology, 2022, 40(6): 922-932.
张君霞, 黄武斌, 杨秀梅, 刘维成, 周子涵, 沙宏娥. 陇东半干旱区一次特大暴雨事件的降水极端性分析[J]. 干旱气象, 2022, 40(6): 922-932.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2022)-06-0922
Fig.1 Spatial distribution of accumulated precipitation from 20:00 BST 14 to 20:00 BST 15 July 2022 (a, Unit: mm) and terrain elevation (the color shaded, Unit: m) and meteorological stations (b) in Qingyang (the rectangular regions for position of strong rainfall center)
Fig.2 The distribution of stations with maximum cumulative precipitation from 20:00 BST 14 to 20:00 BST 15 July 2022 in Qingyang since the establishment of each station
Fig.3 The accumulative precipitation on 14 to 15 July 2022 and historical mean precipitation in flood season and July at the top 10 stations in terms of the cumulative precipitation during the severe torrential rain process in Qingyang
Fig.4 The distribution of accumulative precipitation in 12 (a), 6 (b) and 3 (c) hours from 20:00 BST 14 to 20:00 BST 15 July 2022 at stations with maximum cumulative precipitation during historical same period since the establishment in Qingyang (Unit: mm)
Fig.5 Spatial distribution of maximum hourly precipitation (a, Unit: mm) and its contribution rate to the total precipitation(b, Unit: %) and stations with maximum hourly precipitation since the establishment of station (c), and station numbers occurring maximum hourly precipitation (d) from 20:00 BST 14 to 20:00 BST 15 July 2022
Fig.6 The variation of hourly precipitation of short-term heavy rain at the typical representative stations from 21:00 BST 14 to 20:00 BST 15 July 2022 in Qingyang
Fig.7 The distribution of occurring times (a, Unit: times) and duration (b, Unit: h) of short-term heavy rain and stations with extreme rainfall intensity of short-term heavy rain (c) from 20:00 BST 14 to 20:00 BST 15 July 2022, and the distribution of longest duration of short-term heavy rain before this process (d, Unit: h) in Qingyang
Fig.9 The longitude-time section along 36.15°N (a) and latitude-time section along 107.6°E (b) of hourly precipitation from 21:00 BST 14 to 20:00 BST 15 July 2022 in Qingyang (Unit: mm)
Fig.10 The longitude-time section along 36.15°N (a) and latitude-time section along 107.6°E (b) of 10-minitue precipitation from 21:00 BST 14 to 20:00 BST 15 July 2022 in Qingyang (Unit: mm)
Fig.11 Minutely precipitation evolution at typical representative stations from 00:00 BST to 09:00 BST (a) and from 15:00 BST to 20:00 BST (b) on 15 July 2022
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