DR柱;粒子識(shí)別算法;微物理;熱動(dòng)力"/> DR”(差分反射率因子柱)的演變特征,利用X波段雙偏振雷達(dá)數(shù)據(jù),結(jié)合地面觀測(cè)資料與再分析資料對(duì)2018年5月8日的一次孤立單體降雹過(guò)程進(jìn)行了分析,結(jié)果表明:①孤立單體發(fā)展階段,“ZDR柱”躍增,躍增后0 ℃層以上過(guò)冷水?dāng)?shù)量與高密度霰數(shù)量驟增,變化率分別為26.7庫(kù)/min與11.8庫(kù)/min。成熟階段,“ZDR柱”深度延展至接近-20 ℃層,單體內(nèi)微物理反應(yīng)加劇,冰雹數(shù)量驟增,生成速率為105.8庫(kù)/min。“ZDR柱”轉(zhuǎn)化面積為210庫(kù)的“ZDR洞”(差分反射率因子洞)(ZDR<1),可以指示地面降雹位置。②降雹發(fā)生在“ZDR柱”崩塌后,固體降水物的拖拽作用使得“ZDR柱”高度降至-10 ℃層以下。小雹下落至0 ℃層以下時(shí)融化,表層形成水膜,導(dǎo)致降雹時(shí)近地面出現(xiàn)ZDR大值區(qū)。③孤立單體內(nèi)微物理過(guò)程與熱動(dòng)力過(guò)程相互作用,促進(jìn)了“ZDR柱”的生成發(fā)展。本文針對(duì)一次孤立單體雹暴過(guò)程不同階段“ZDR柱”的演變特征進(jìn)行了分析,并建立了相對(duì)應(yīng)的雹暴模型,對(duì)當(dāng)?shù)乇⒌念A(yù)警及防治有重要的意義。"/>
一次孤立單體雹暴過(guò)程“ZDR柱”演變特征分析
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國(guó)家自然科學(xué)基金項(xiàng)目(41875169)、貴州省科技計(jì)劃項(xiàng)目黔科合支撐([2019]2387號(hào))、四川省重點(diǎn)研發(fā)項(xiàng)目(2022YFS0545)、云南省重點(diǎn)研發(fā)項(xiàng)目(202203AC100006)資助


Analysis of Evolution Characteristics of “ZDR Column”in an Isolated Hail Storm
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    摘要:

    為了研究孤立單體內(nèi)“ZDR”(差分反射率因子柱)的演變特征,利用X波段雙偏振雷達(dá)數(shù)據(jù),結(jié)合地面觀測(cè)資料與再分析資料對(duì)2018年5月8日的一次孤立單體降雹過(guò)程進(jìn)行了分析,結(jié)果表明:①孤立單體發(fā)展階段,“ZDR柱”躍增,躍增后0 ℃層以上過(guò)冷水?dāng)?shù)量與高密度霰數(shù)量驟增,變化率分別為26.7庫(kù)/min與11.8庫(kù)/min。成熟階段,“ZDR柱”深度延展至接近-20 ℃層,單體內(nèi)微物理反應(yīng)加劇,冰雹數(shù)量驟增,生成速率為105.8庫(kù)/min。“ZDR柱”轉(zhuǎn)化面積為210庫(kù)的“ZDR洞”(差分反射率因子洞)(ZDR<1),可以指示地面降雹位置。②降雹發(fā)生在“ZDR柱”崩塌后,固體降水物的拖拽作用使得“ZDR柱”高度降至-10 ℃層以下。小雹下落至0 ℃層以下時(shí)融化,表層形成水膜,導(dǎo)致降雹時(shí)近地面出現(xiàn)ZDR大值區(qū)。③孤立單體內(nèi)微物理過(guò)程與熱動(dòng)力過(guò)程相互作用,促進(jìn)了“ZDR柱”的生成發(fā)展。本文針對(duì)一次孤立單體雹暴過(guò)程不同階段“ZDR柱”的演變特征進(jìn)行了分析,并建立了相對(duì)應(yīng)的雹暴模型,對(duì)當(dāng)?shù)乇⒌念A(yù)警及防治有重要的意義。

    Abstract:

    In order to study the evolution characteristics of the ZDR column in an isolated cell, the hailing process of an isolated cell on May 8, 2018, is analyzed by using X-band dual-polarization radar data combined with ground observation data and reanalysis data. The results show that: (1) In the development stage of an isolated cell, the ZDR column increased rapidly. After the jump, the number of SWAs (Supercooled Water Areas) and HDGs (High Density Graupels) above the 0 ℃ layer increased sharply, and the change rates were 26.7 bins per minute and 11.8 bins per minute, respectively. In the mature stage, the depth of the ZDR column extended to the nearly -20 ℃ layer, the microphysical reaction in the monomer intensified, the number of hail increased rapidly, and the generation rate was 105.8 bin/min. The ZDR column was transformed into a ZDR hole (ZDR<1) with an area of 210 bins, which indicates the ground hail location. (2) Hail occurred after the collapse of the ZDR column. The height of the ZDR column dropped below -10 ℃ due to the dragging effect of solid precipitation. When the small hail fell below the layer of 0 ℃, it melted and formed a water film on the surface, resulting in the ZDR large value area near the ground during the hail fall. (3) The interaction between the microphysical process and thermal dynamic in the isolated cell promoted the formation and development of the ZDR column. In this paper, the evolution characteristics of the ZDR column in different stages of an isolated hail storm are analyzed, and the corresponding hail storm model is established, which is of great significance to the early warning and prevention of local hails.

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沈雨,周筠珺,鄒書(shū)平,楊哲,曾勇.一次孤立單體雹暴過(guò)程“ZDR柱”演變特征分析[J].氣象科技,2023,51(1):104~114

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  • 收稿日期:2021-11-01
  • 最后修改日期:2022-11-21
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  • 在線發(fā)布日期: 2023-03-03
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