青島機場一次冰雹過程的雙偏振雷達分析
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中國氣象局蘭州干旱氣象研究所基金項目(KYS2022BSKY01)資助


Dual-Polarization Radar Analysis of a Hail Process at Qingdao Airport
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    摘要:

    利用常規氣象觀測站點資料、探空資料、青島S波段多普勒和雙偏振雷達資料對2023年7月8日下午青島機場一次對流單體冰雹過程天氣背景以及雷達回波特征進行分析。結果表明:此次冰雹過程是在500 hPa強西風帶、冷渦槽的共同作用下發生的,具有很強的局地性。整層大氣具有強的不穩定性,上干下濕特征明顯,低層垂直風切變強度中等,深層垂直風切變較強,0~6 km風矢量差達到21 m/s,高低空溫差較大,濕球溫度0 ℃高度為4 km。雷達回波具有高聳的強回波、有界弱回波區、回波懸垂和三體散射結構,同時中層4~8 km的高度處有明顯中氣旋結構,氣旋直徑約4 km,輻合層厚度約為3.2 km,高層出現速度輻散,這些均為典型雹暴的雷達特征。單體的垂直液態水含量(C-VIL)和垂直液態水含量(VIL)密度的大值能夠很好對應冰雹粒子,C-VIL突變還能作為預報冰雹和大風參考指標,C-VIL躍增出現比青島機場降雹提前30 min,驟降出現比青島機場大風出現提前7 min。這次冰雹過程,雙偏振雷達差分反射率因子ZDR和相關系數ρhv能有效區分冰雹和強降水,而差分相位常數KDP大值區對應大雨或融化的冰雹,需要結合其他參量進一步判斷粒子形態。這次冰雹過程出現了明顯的ZDRKDP柱結構,ZDR柱高于KDP柱,ZDR柱對應較強的上升運動,與速度圖上的中氣旋位置相對應,KDP柱對應著較明顯的下沉氣流。分析的結果能為青島機場的冰雹短臨預報提供一定的參考,也對于實際應用雙偏振雷達產品有一定的指示意義。

    Abstract:

    Using the data from conventional meteorological observation stations, sounding data, and S-band Doppler and dual-polarization radar data from Qingdao, the weather background and radar echo characteristics of a convective hail event at Qingdao Airport on the afternoon of July 8, 2023 are analyzed. The results show that the hail event occurred under the combined action of a strong westerly wind belt at 500 hPa and a cold vortex trough, with strong local characteristics. The entire atmosphere had strong instability, with obvious characteristics of dryness in the upper layer and wetness in the lower layer. The vertical wind shear intensity in the lower layer was moderate, while the vertical wind shear intensity in the deep layer was strong. The wind vector difference between 0 and 6 km reached 21 m/s, and the temperature difference between high and low altitudes was large. The height at wet bulb temperature 0 ℃ was 4 km. The radar echoes had high-rise strong echoes, bounded weak echo areas, echo hangings, and three-body scattering structures. At the same time, there was a clear mesocyclone structure at an altitude of 4-8 km in the middle layer, with a diameter of about 4 km and a thickness of about 3.2 km in the convergence layer. There was a velocity divergence in the upper layer. These were all typical radar characteristics of hailstorms. The large values of C-VIL and VIL density could well correspond to hail particles, and the C-VIL mutation could also be used as a reference index for forecasting hail and strong winds. The C-VIL jump occurred 30 minutes before the hail at Qingdao Airport, and the sudden drop occurred 7 minutes before the strong wind at Qingdao Airport. During this hail process, the dual-polarisation radar parameters ZDR and ρhv could effectively distinguish hail and strong precipitation, while the KDP large value area corresponded to heavy rain or melted hail. It was necessary to combine other parameters to further determine the particle morphology. This hail process showed obvious ZDR and KDP column structures, with the ZDR column higher than the KDP column. The ZDR column corresponded to strong upward motion, which corresponded to the location of the mesocyclone on the velocity diagram, while the KDP column corresponded to a more obvious downdraft. The analysis results can provide some reference for short-term and imminent forecasts of hail at Qingdao Airport, and also have some instructive significance for the practical application of dual-polarisation radar products.

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劉源,陳思遠,張鈺欣,房云龍,趙京華.青島機場一次冰雹過程的雙偏振雷達分析[J].氣象科技,2024,52(4):549~559

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  • 收稿日期:2023-09-01
  • 定稿日期:2024-03-27
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  • 在線發布日期: 2024-08-28
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