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Analysis of Temporal and Spatial Variation Characteristics of Short-term Heavy Precipitation in Chongqing Based on Different Landforms
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Lan KUANG1, Mao-ju TIAN1, Qiang LI2, Yue PANG2, Xiang LIU3, Xun TAO4
Water Resources and Power | 2023, 41(4) : 1 - 4
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Water Resources and Power | 2023, 41(4): 1-4
HYDROLOGY, WATER RESOURCES AND ENVIRONMENT
Analysis of Temporal and Spatial Variation Characteristics of Short-term Heavy Precipitation in Chongqing Based on Different Landforms
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Lan KUANG1, Mao-ju TIAN1, Qiang LI2, Yue PANG2, Xiang LIU3, Xun TAO4
Affiliations
  • 1.Chongqing Qijiang Meteorological Bureau, Chongqing 401420, China
  • 2.Chongqing Meteorological Observatory, Chongqing 401147, China
  • 3.Chongqing Meteorological Service Center, Chongqing 401147, China
  • 4.Chongqing Jiangjin Meteorological Bureau, Chongqing 402260, China
Published: 2023-04-25 doi: 10.20040/j.cnki.1000-7709.2023.20221370
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Based on the SRTM digital elevation DEM model, using the hourly precipitation data of Chongqing from May to September 2017 to 2021, this paper analyzed the temporal and spatial distribution characteristics of short-term heavy precipitation under different terrains in Chongqing, and discussed the relationship between the frequency and intensity of short-term heavy precipitation and topographic factors. The results show that the spatial distribution of short-term heavy precipitation in Chongqing is uneven. The overall average frequency high value area of the previous year and stations ≥ 60mm/h are mainly located near Huaying Mountain in Northwest Chongqing, Daba Mountain in Northeast Chongqing and Wuling Mountain in Southeast Chongqing; For the station average frequency of short-term heavy precipitation in Chongqing, the monthly variation shows a significant single peak type, and the frequency is the most in July; The diurnal variation is bimodal, with the main peak occurring most frequently at 03:00-05:00 and the secondary peak occurring more frequently at 16:00-19:00. The frequencies of the north and west slopes are slightly more than those of the other slopes. The frequency of flat slope and gentle slope is more than that of other slopes. The frequency of 500-1 000 m and > 1500 m is more than that of other altitudes; The fluctuation ≤30 m and 30-200 m are more frequent than other fluctuations; When slope ≤15°, altitude ≤1 000 m, and undulation ≤200 m, stations with precipitation intensity ≥100 mm/h appear, indicating that appropriate mountain topography is conducive to the increase of short-time heavy rainfall intensity. The research results can provide reference for near early warning, disaster prevention and reduction of short-term heavy precipitation in Chongqing.

intensive observation  /  Chongqing  /  mountainous terrain  /  short-term heavy precipitation  /  temporal and spatial distribution
Lan KUANG, Mao-ju TIAN, Qiang LI, Yue PANG, Xiang LIU, Xun TAO. Analysis of Temporal and Spatial Variation Characteristics of Short-term Heavy Precipitation in Chongqing Based on Different Landforms[J]. Water Resources and Power, 2023 , 41 (4) : 1 -4 . DOI: 10.20040/j.cnki.1000-7709.2023.20221370
Year 2023 volume 41 Issue 4
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Article Info
doi: 10.20040/j.cnki.1000-7709.2023.20221370
  • Receive Date:2022-07-05
  • Online Date:2026-01-27
  • Published:2023-04-25
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History
  • Received:2022-07-05
  • Revised:2022-08-05
Funding
Affiliations
    1.Chongqing Qijiang Meteorological Bureau, Chongqing 401420, China
    2.Chongqing Meteorological Observatory, Chongqing 401147, China
    3.Chongqing Meteorological Service Center, Chongqing 401147, China
    4.Chongqing Jiangjin Meteorological Bureau, Chongqing 402260, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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