上海二次温室大棚区强尘卷风的成因分析
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国家自然科学基金资助项目(41475040)


Analysis of the causes of strong dust devil in the secondary greenhouse area of Shanghai
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    摘要:

    尘卷风是近地面气层中的小旋风,使沙尘或其他细小物体随风卷起而形成的一种天气现象。2011年10月27日11时10分和2015年9月13日11时12分发生于上海地区的两次强尘卷风天气过程(北京时,下同)均造成了不同程度的灾害。两次尘卷风均发生在温室大棚区,其下垫面性质和干旱区裸露地面和水泥沥青城市地面极不相同,因此了解其发生原因很有必要。本文利用常规天气图、温度对数压力图、100 m以下5层铁塔风和温度、微波辐射仪以及温室大棚基地自动气象站等资料对这两次尘卷风过程进行了分析。发现.在常规探空都未探测到明显的超绝热现象,但在铁塔观测的地表面层温度垂直廓线结合微波辐射仪及自动气象站等资料揭示了尘卷风发生时近地面气层都具备了超绝热条件。尘卷风发生前后10:00-12:00的10~70 m温度垂直递减率γ平均达1.58℃/100 m,极大值达2.33℃/100 m,为干绝热递减率的两倍还多。上海地区10座铁塔测风网获得的10、30、50、70 m近地层风场的旋转和辐合特征揭示了尘卷风旋转的角动量来源。通过分析500、700、850 hPa天气形势探讨了有利于发生尘卷风的大尺度环流条件为尘卷风预报提供参考。最后对这两次尘卷风发生在温室大棚区域而不是自然农田的机理提出了初步看法供进一步讨论。

    Abstract:

    A dust devil is a weather phenomenon caused by small cyclones in the near-surface gas layer that make sand or other small objects roll up with the wind. At 11∶10 on October 27, 2011 and at 11∶12 on September 13, 2015 respectively, two strong dust devil weather events that occurred in Shanghai (Beijing time, the same below) caused different levels of disasters. Both dust devils occurred in the greenhouse area, the nature of the underlying surface of which is very different from that of exposed ground in the arid area and cement asphalt road surface in the city. Therefore, it is necessary to understand the cause. In this paper, the two dust devil processes are analyzed by using data from conventional weather maps, temperature logarithmic pressure maps, five-story tower wind and temperature below 100 m, microwave radiometers, and automatic weather stations in greenhouses, etc. It was found that no obvious super-adiabatic phenomenon was detected in the conventional sounding, but the vertical profile of the surface layer temperature observed by the tower combined with data from the microwave radiometer and the automatic weather station revealed that the near-surface gas layers were both equipped with super adiabatic conditions when the dust devils occurred. The mean vertical lapse rate of temperature γ before and after the occurrence of dust devils (10∶00—12∶00) reached 1.58 ℃/100 m, and the maximum value reached 2.33 ℃/100 m, which is more than twice the dry adiabatic lapse rate. The swirling and convergence characteristics of the 10 m, 30 m, 50 m, and 70 m near-surface wind fields obtained from the ten tower wind measurement networks in Shanghai revealed the source of angular momentum of the dust devil swirling. By analyzing the weather conditions of 500, 700 and 850 hPa, the large-scale circulation conditions favorable to the occurrence of dust devils are discussed to provide reference for dust devil forecasting. Finally, a preliminary view of the mechanism of the occurrence of the two dust devils in the greenhouse area rather than in the natural farmland is proposed for further discussion.

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戴蔚明,胡平,荣裕良,马忠芬,顾忠良.上海二次温室大棚区强尘卷风的成因分析.气象科学,2019,39(1):117-128 DAI Weiming, HU Ping, RONG Yuliang, MA Zhongfen, GU Zhongliang. Analysis of the causes of strong dust devil in the secondary greenhouse area of Shanghai. Journal of the Meteorological Sciences,2019,39(1):117-128

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  • 收稿日期:2017-05-02
  • 最后修改日期:2017-09-25
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  • 在线发布日期: 2019-03-18
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