高级搜索

基于三波长拉曼-米散射激光雷达的武汉地区卷云粒子光学参数特征

Optical parameters of cirrus particles in Wuhan based on three-wavelength raman-mie scattering lidar

  • 摘要: 为识别卷云光学特征,基于2023年10—12月武汉国家基本气象站三波长拉曼-米散射激光雷达的连续观测资料,选取武汉地区2023年11月一次典型卷云过程为例进行分析。结果表明,此次卷云过程中卷云平均云底高度为7.0 km,并呈现夜间缓慢降低、白天逐渐升高的变化趋势,期间355 nm、532 nm平均雷达比分别为40.6 Sr和59.3 Sr。结合后向散射系数和退偏振比识别卷云粒子相态,过程中云底和云顶三个波长间后向散射系数差异小,且退偏振比在0.35以上,以非球形大粒子为主,而云内355 nm和532 nm后向散射系数明显高于1 064 nm,且退偏振比较小,多为球形小粒子,云团自下而上表现出冰晶-过冷水-冰晶的结构分布特征。

     

    Abstract: In order to identify the optical characteristics of cirrus clouds, a typical cirrus event in Wuhan in November 2023 was selected as an example for analysis based on the continuous observation data of the three-wavelength raman-mie scattering lidar in Wuhan National Basic Meteorological Station from October to December 2023. The results are as follows. The average cloud base height of cirrus during this event was 7.0 km, and it showed a trend of slowly decreasing at night and gradually increasing during the day. During this period, the average lidar ratios of 355 nm and 532 nm were 40.6 Sr and 59.3 Sr, respectively. The phases of cirrus particles were identified by combining the backscattering coefficient and depolarization ratio. During the event, the differences in backscattering coefficients between the three wavelengths of the cloud base and the cloud top were small, and the depolarization ratios were above 0.35, which meant that cirrus particles were mainly non-spherical large particles. The backscattering coefficients of 355 nm and 532 nm in the cloud were significantly higher than 1 064 nm, and the smaller depolarization ratios indicated that there were more spherical particles in the cloud. So the structure distribution characteristic of the cirrus was ice crystal-supercooled water-ice crystal from the bottom up.

     

/

返回文章
返回