巴音布鲁克区域大气可降水量变化特征及其与降水的关系OA
Variation characteristics of precipitable water vapor and its relationship with precipitation in the Bayanbuluk area
研究大气可降水量(PWV)与降水之间的演变关系,有助于揭示区域云降水物理特征和水分循环机制,为防灾减灾、水资源利用和生态保护提供关键技术支撑.以对气候变化敏感的巴音布鲁克高寒山区为研究区,基于2021年1月—2025年12月逐时的地基GPS大气可降水量资料及降水数据,研究了高寒山区PWV的时间变化特征及其与降水的关联机制.结果表明:(1)月尺度中PWV与降水量均呈单峰型分布,两者高值时期均主要出现在6-8月,低谷期在12月至翌年2月.此外,日尺度上随着PWV增长,累计降水量呈显著增加趋势(P<0.001),说明研究区的PWV与降水量具有密切协同变化特征.(2)在不同量级的降水过程事件中,小雨的PWV峰值多在降水前6~8 h出现,而中雨及大雨较为一致,主要在降水前3~7 h出现,说明随着PWV峰值出现时刻越接近降水开始时刻,更易出现过程量级较大的降水事件.(3)在不同降水开始时的雨强量级上,PWV峰值在降水前的出现时间差异较大,其中R≤2.0 mm和4.1 mm≤R≤6.0 mm的量级均在降水前6~10 h,2.1 mm≤R≤4.0 mm量级则多在5~7 h,而R≥6.1 mm量级在3~6 h,说明PWV峰值出现时刻越接近降水开始时刻,降水初始时刻的小时降水量易偏大.(4)降水持续时间在5h以内,降水转化率普遍较大,均在8.0%以上,而5~14 h内,降水转化率普遍较低,多在5.0%以下.此外,降水过程量级以中雨的平均降水转化率最高,为11.3%,而雨强量级以下午易发的R≥6.1 mm最多,达到了40.0%以上.
Investigating the relationship between atmospheric precipitable water vapor(PWV)and precipitation is helpful not only for revealing regional cloud-precipitation physical characteristics and water cycle mechanisms,but also for providing key technical support for disaster prevention and mitigation,water resource utilization,and ecological protection.Based on hourly ground-based GPS atmospheric PWV data and precipitation data from Jan-uary 2021 to December 2025,and focusing on the climate-sensitive alpine region of Bayanbuluk as the study ar-ea,the temporal variation characteristics of PWV and its correlation mechanisms with precipitation were investi-gated.The results show that:(1)Both PWV and precipitation exhibit unimodal distributions at the monthly scale,with peak values occurring from June to August and troughs from December to February.At the daily scale,cumulative precipitation shows a notable increasing trend with PWV growth,indicating close synergistic variations between PWV and precipitation in the study area.(2)Before the occurrence of light rain events,the PWV peak usually appears 6 to 8 h earlier,while for moderate rain and heavy rain events,the lead time is rela-tively consistent,mainly 3 to 7 h before precipitation onset.This indicates that as the interval between the PWV peak and the start of precipitation becomes shorter,events with larger precipitation magnitudes are more likely to occur.(3)For events with rainfall intensities of R≤2.0 mm and 4.1 mm≤R≤6.0 mm at precipitation onset,the PWV peak mostly occurs 6 to 10 h before precipitation;for the 2.1 mm≤R≤4.0 mm range,it mostly occurs 5 to 7 h before;and for R≥6.1 mm,the PWV peak mostly occurs 3 to 6 h before.This indicates that as the interval be-tween the PWV peak and precipitation onset becomes shorter,the hourly precipitation at the initial moment tends to be larger.(4)When the duration of precipitation is less than 5 h,the precipitation conversion rate is generally high,exceeding 8.0%,while for durations of 5-14 h,the conversion rate is generally low,mostly less than 5.0%.In addition,the average precipitation conversion rate is highest for moderate rainfall events and R≥6.1 mm rain-fall intensity events in the afternoon,exceeding 11.3%and 40.0%,respectively.
刁鹏;李圆圆;李刚;杨波
巴音郭楞蒙古自治州气象局,新疆 库尔勒 841000||新疆人工影响天气工程技术研究中心,新疆 乌鲁木齐 830002新疆人工影响天气工程技术研究中心,新疆 乌鲁木齐 830002||新疆人工影响天气中心,新疆 乌鲁木齐 830002巴音郭楞蒙古自治州气象局,新疆 库尔勒 841000||新疆人工影响天气工程技术研究中心,新疆 乌鲁木齐 830002巴音郭楞蒙古自治州气象局,新疆 库尔勒 841000||新疆人工影响天气工程技术研究中心,新疆 乌鲁木齐 830002
大气可降水量降水量降水转化率变化特征巴音布鲁克区域
precipitable water vaporprecipitationprecipitation conversion efficientvariation characteristicsBayanbuluke area
《干旱区研究》 2026 (6)
1113-1124,12
新疆维吾尔自治区重点研发计划项目(2023B03019-1)国家重点研发计划项目(2024YFF1308203)新疆维吾尔自治区气象局创新发展基金项目(MS202612)中国气象局—成都信息工程大学人工影响天气联合研究中心开放课题(2025RGYXTQ019)巴音郭楞蒙古自治州气象局科研基金课题(202502)
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