一次東北冷渦過程的宏微觀物理特征分析
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中國氣象局云霧物理環境重點開放實驗室開放課題(2019Z1605)資助


Cloud Microphysical Characteristic Analysis of a Northeast Cold Vortex Process
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    摘要:

    利用2019年5月20日機載DMT和SPEC粒子測量系統獲取的飛機云微物理探測資料,結合高空、地面、衛星云圖產品等常規氣象數據,分析了東北冷渦在發展成熟期的云宏微觀結構特征。結果表明:飛機探測區域為冷性層積混合云,云水充沛。云粒子探頭(CDP)和二維云粒子圖像探頭(CIP)探測到的最大粒子數濃度分別為362.10 cm-3、191.08 L-1,液態含水量變化范圍為0~0.88 g/m3;CDP粒子譜呈指數型下降,譜寬較窄;CIP粒子譜呈雙峰結構。云粒子圖像探測儀CPI表明,層積云上部主要為冰雪晶粒子,以冰晶的核化和凝華增長為主;中上部粒子主要為小冰晶形態,也有冰晶聚合體和枝狀冰晶;中下部是過冷水和冰晶粒子的共存區,過冷水較為豐富。

    Abstract:

    Based on the data from meteorological satellites, the macrophysical and microphysical characteristics of the stratocumulus cloud system on 20 May 2019 are analyzed by using the cloud physical data from DMT (Droplet Measurement Technologies) and SPEC (Stratton Park Engineering Compang). The results show that the maximum particle number concentrations of CDP (Cloud Droplet Probe) and CIP(Cloud Imaging Probe) were 362.10 cm-3 and 191.08 L-1, respectively. The content of liquid water ranged from 0 to 0.88 g/m3. The spectral distribution shows that the particle spectra of CDP and CIP exhibited exponentialtype decline. The spectral width of the CDP particle spectrum is narrow. The spectral width of the CIP particle spectrum is narrow on the top of clouds while the lower layer is wide. The observed results of CPI show that the upper stratocumulus was mainly composed of ice and snow particles, which were dominated by nucleation and coagulation growth of ice crystals. The upper and middle particles were mainly composed of small ice crystals, some ice crystal polymers and dendritic ice crystals. The middle and lower parts were composed of supercooled water and ice crystal particles, with rich supercooled water.

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李冬楠,劉星光,高倩楠,袁潮,李鵬,安英玉.一次東北冷渦過程的宏微觀物理特征分析[J].氣象科技,2021,49(2):227~234

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歷史
  • 收稿日期:2020-04-09
  • 定稿日期:2020-06-22
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  • 在線發布日期: 2021-04-25
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