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首页|期刊导航|高原气象|青藏高原东南缘九龙地区风廓线雷达与无线电探空资料的对比分析

青藏高原东南缘九龙地区风廓线雷达与无线电探空资料的对比分析

刘莹 曾波 陈莹 陈朝平 周秋雪 胡迪 邓佳

高原气象2026,Vol.45Issue(4):1209-1220,12.
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高原气象2026,Vol.45Issue(4):1209-1220,12.DOI:10.7522/j.issn.1000-0534.2025.00127

青藏高原东南缘九龙地区风廓线雷达与无线电探空资料的对比分析

Comparative analysis of wind profiler radar and radiosonde data in the Jiulong Area on the southeastern margin of the Qinghai-Xizang Plateau

刘莹 1曾波 2陈莹 3陈朝平 3周秋雪 3胡迪 3邓佳3

作者信息

  • 1. 中国气象局成都高原气象研究所 高原与盆地暴雨旱涝灾害四川省重点实验室,四川 成都 610213||四川省气象台,四川 成都 610072
  • 2. 中国气象局成都高原气象研究所 高原与盆地暴雨旱涝灾害四川省重点实验室,四川 成都 610213||中国气象科学研究院 青藏高原气象研究院,北京 100081
  • 3. 四川省气象台,四川 成都 610072
  • 折叠

摘要

Abstract

In order to verify the availability of wind profiler radar(WPR)data in in the Jiulong Area on the southeastern margin of the Qinghai-Xizang Plateau,improve the application value of WPR data in plateau area.This study systematically compares horizontal wind profiles from WPR and Southwest Vortex radiosonde obser-vations with four times daily[02:00(Beijing Time,the same as after),08:00,14:00,20:00]of the Jiulong Area from 2015 to 2022.Two temporal matching strategies(single-timepoint and multi-timepoint smoothed data)were employed to assess data consistency.The results reveal:(1)the WPR data acquisition rate exhibits a verti-cally non-monotonic pattern(decline-rise-sharp decrease),with diurnally varying effective detection heights(valid data ratio:0.8),peaking at 20:00 and reaching minimum at 08:00.(2)The WPR and radiosonde data showed strong correlation,which was further improved by temporally averaged WPR data.(3)Vertical stratifica-tion is evident,upper-level WPR-radiosonde correlations strengthen with altitude,whereas lower-level wind components show superior stability.Temporally averaged data significantly improve the quality of u and v compo-nents below 3000 m,but only marginally improve wind direction estimates.(4)The differences in the u,v com-ponents and wind direction between both WPR schemes and the radiosonde data approximately follow a normal distribution.Comparative analysis across different times indicated that the data quality of the u and v components was optimal at 08:00,whereas the largest errors in wind direction occurred at 14:00.(5)The frequency distribu-tions of wind direction and speed from both WPR schemes were generally consistent with those from the radio-sonde.The temporally averaged WPR data showed closer agreement with the radiosonde derived winds.Howev-er,both schemes slightly underestimated the frequency of southeasterly winds compared to the radiosonde,with this discrepancy being most pronounced at 14:00.

关键词

九龙地区/风廓线雷达/探空/风场/资料评估

Key words

Jiulong area/wind profiler radar/radiosonde/wind/data evaluation

分类

天文与地球科学

引用本文复制引用

刘莹,曾波,陈莹,陈朝平,周秋雪,胡迪,邓佳..青藏高原东南缘九龙地区风廓线雷达与无线电探空资料的对比分析[J].高原气象,2026,45(4):1209-1220,12.

基金项目

国家自然科学基金联合基金项目(U2242202) (U2242202)

西藏科技厅重大专项(XZ202402ZD0006) (XZ202402ZD0006)

四川省科技计划项目(2025ZNSF-SC0334) (2025ZNSF-SC0334)

国家重点研发计划项目(2023YFC3007502) (2023YFC3007502)

国家重点研发计划项目(2022YFC3003902) (2022YFC3003902)

高原与盆地暴雨旱涝灾害四川省重点实验室研究型业务重点专项(SCQXKJYJXZD202402) (SCQXKJYJXZD202402)

高原气象

1000-0534

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