干旱气象 ›› 2025, Vol. 43 ›› Issue (6): 931-938.DOI: 10.11755/j.issn.1006-7639-2025-06-0931

• 论文 • 上一篇    下一篇

贵州梵净山汛期降水日变化特征

陈桂峰1(), 张驰3, 乔琪2, 谢清霞2(), 邓苏1, 白琴琴1   

  1. 1.贵州省江口县气象局贵州 江口 554400
    2.贵州省气象台贵州 贵阳 550002
    3.重庆市气候中心重庆 401147
  • 收稿日期:2025-03-28 修回日期:2025-06-18 出版日期:2025-12-31 发布日期:2026-01-19
  • 通讯作者: 谢清霞(1980—),女,高级工程师,主要从事中短期天气预报和研究。E-mail: 66506485@qq.com
  • 作者简介:陈桂峰(1998—),男,助理工程师,主要从事短临天气预报研究。E-mail: 739072153@qq.com
  • 基金资助:
    “梵净山东侧汛期降水日变化及区域数值模式的精细评估和误差分析研究”项目(ZJLY202415-GZ01);“基于改进YOLO模型的云粒子形态识别算法研究”项目(2024CPML-C011)

Diurnal variation of precipitation in flood season in Fanjing Mountain in Guizhou

CHEN Guifeng1(), ZHANG Chi3, QIAO Qi2, XIE Qingxia2(), DENG Su1, BAI Qinqin1   

  1. 1. Jiangkou Meteorological Bureau of Guizhou ProvinceJiangkou 554400, Guizhou, China
    2. Guizhou Provincial Meteorological ObservatoryGuiyang 550002, China
    3. Chongqing Climate CenterChongqing 401147, China
  • Received:2025-03-28 Revised:2025-06-18 Online:2025-12-31 Published:2026-01-19

摘要:

为加深对山地复杂地形区的降水规律认识,利用贵州梵净山东侧不同海拔高度的3个气象观测站2022—2023年汛期5—10月逐小时降水资料,分析山脚、山腰和山顶站降水日变化特征。结果表明:夜间至早晨降水量和降水强度随海拔升高而增大,午后至傍晚两者随海拔升高而减小;山脚站和山腰站降水量大值时段出现于午后到傍晚,山顶站则集中于凌晨到早晨;3站降水量主要来源于持续2~18 h的降水事件,山顶站持续8 h以内的降水事件其降水量均表现为夜间大于白天,山脚站和山腰站这一特征仅体现在持续3 h以内的降水事件中;降水高发时段随海拔升高呈现系统性推迟,从山脚站的夜间至上午,经山腰站的夜间到中午,过渡到山顶站的中午到凌晨,表现出“从上午到中午向凌晨传播”的趋势。短历时强降水(降水量≥25 mm)多出现在早晨且降水频次最多,长历时降水的降水量占比最大。

关键词: 梵净山, 海拔高度, 山地降水, 日变化

Abstract:

To deepen the understanding of precipitation patterns in complex mountainous terrain, hourly precipitation data from three meteorological observation stations at different altitudes on the eastern side of the Fanjing Mountain in Guizhou Province in the flood season from May to October during 2022-2023 were used to analyze the diurnal variation characteristics of precipitation at the foot, mid-slope and summit stations. The results show that the amount and intensity of precipitation from night to morning increase with increasing altitude, while both decrease with increasing altitude from afternoon to evening. The periods with the large precipitation amount at stations on the foot and middle of the mountain occur from the late afternoon to evening, while at the summit station it concentrates from the early morning to morning. The precipitation at three stations mainly originates from rainfall events lasting from 2 to 18 hours. At the summit station, the precipitation amount during rainfall events lasting less than 8 hours is greater at night than during the day, while at the foot and mid-mountain stations, this characteristic is only observed in rainfall events lasting less than 3 hours.The peak period of precipitation shows a systematic delay with altitude increasing. From the night to the morning at the station at the foot of the mountain, then from the night to the noon at the station on the middle of the mountain, and finally transitioning from the noon to the early morning at the top station of the mountain, it exhibits a trend of “spreading from the morning to the noon and then to the early morning”. Short duration heavy precipitation (with precipitation amount greater than or equal to 25 mm) mostly occurs in the morning and has the highest frequency, while long duration precipitation has the highest proportion of precipitation amount.

Key words: the Fanjing Mountain, altitudes, mountain precipitation, diurnal variation

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