温度湿度同步探测的拉曼激光雷达系统研制与性能验证

Development and performance validation of a Raman lidar system for simultaneous temperature and humidity detection

  • 摘要: 在全球极端天气事件频发的气候背景下,温度湿度精细化垂直廓线的监测需求迫切,为更好地实现激光雷达的探测精准度和验证长时间观测的稳定性,推动其业务化应用,设计研制了一套温度湿度同步探测激光雷达系统。基于低能量355 nm发射光源与多级分光技术,通过转动/振动拉曼散射信号反演,实现了0.1~6 km垂直范围内温度、相对湿度及水汽混合比的高时空分辨率连续探测。62组探空数据比对验证显示,在0.1~2 km、2~4 km和4~6 km高度区间,温度绝对平均误差分别为0.877 K、0.922 K和1.551 K,相对湿度误差分别为5.528%、8.024%和12.312%,水汽混合比误差分别为0.415 g/kg、0.456 g/kg和0.323 g/kg,各高度相关系数大于0.9,数据可靠性显著。实际观测中,该系统可清晰捕捉逆温层的高度与强度演变,揭示降雨前温度湿度垂直演变规律,结合再分析数据验证解析天气现象的形成机制,充分证明了该系统在高精度大气温度湿度探测中的持续监测能力与可靠性。

     

    Abstract:
    Objective Against the backdrop of increasingly frequent extreme weather events worldwide, traditional observation equipment can hardly meet the current demands, and there is an urgent need for fine vertical profiling of atmospheric temperature and humidity. To achieve precise detection and long-term, continuous, and stable lidar observation and to promote its operational application, this study designed and developed a Raman lidar system for simultaneous temperature and humidity detection. The system’s monitoring accuracy and data reliability have been verified to meet the requirements for operational applications.
    Methods The Raman lidar system adopts a low-energy 355 nm laser as the emission source and a multi-stage spectroscopic receiving technology (Fig.1). The overall system is designed with a modular structure (Technical Parameters in Tab.1), enabling high-spatiotemporal-resolution continuous detection of temperature, relative humidity, and water vapor mixing ratio within the vertical range of 0.1-6 km. To conduct error analysis, the lidar data were compared with radiosonde data (Fig.2), and parameters including the absolute mean error, root mean square error, and correlation coefficient of temperature, humidity, and water vapor mixing ratio profiles were calculated. For case analysis, ERA5 reanalysis data were used for mechanism analysis and result verification.
    Results and Discussions The evaluation of 62 concurrent lidar and radiosonde measurements confirmed that the relative errors of temperature (Fig.3), water vapor mixing ratio (Fig.6), and relative humidity (Fig.7) complied with standard meteorological observation requirements. All profiles displayed strong correlations and coherent temporal trends. The mean absolute errors were quantified across three vertical layers: 0.1-2 km, 2-4 km, and 4-6 km. The corresponding errors for temperature were 0.877 K, 0.922 K, and 1.551 K; for relative humidity, 5.528%, 8.024%, and 12.312%; and for water vapor mixing ratio, 0.415 g/kg, 0.456 g/kg, and 0.323 g/kg. A comprehensive statistical analysis of these errors across altitudes and monitoring periods was performed (Tab.2), which helped identify the dominant error sources in each layer. It was found that daytime observations exhibited greater susceptibility to background solar noise, whereas nighttime operations yielded significantly improved data consistency (Fig.4). A comparative assessment against systems reported in the literature (Tab.3) underscored the competitive advantages of the present system. Furthermore, the lidar was deployed to analyze the structure of a temperature inversion layer (Fig.8) and to track the evolution of temperature and humidity profiles preceding a rainfall event (Fig.12). The formation mechanisms of these weather phenomena were elucidated through supporting reanalysis data (Fig.9, Fig.13).
    Conclusions The developed Raman lidar system for simultaneous temperature and humidity detection has demonstrated its capability for long-term, stable operation, successfully obtaining high-resolution vertical profiles of temperature, humidity, and water vapor mixing ratio. Validation against 62 radiosonde launches confirmed the system's accuracy and data consistency across different altitude layers, meeting operational meteorological monitoring requirements. Case studies of temperature inversion and pre-rainfall processes revealed detailed vertical structures and coupling mechanisms between temperature and water vapor. These observations, supported by reanalysis data, verified the formation mechanisms of the studied phenomena, underscoring the lidar's utility in analyzing complex weather dynamics and providing critical evidence for understanding regional severe weather. However, system performance is limited by a significantly degraded signal-to-noise ratio during daytime due to solar background noise, and insufficient detection accuracy above 6 km, which prevents effective coverage of the upper troposphere. Future work will focus on enhancing daytime performance, developing more robust signal processing algorithms, and advancing system automation with standardized quality control to achieve fully operational, long-term observational applications.

     

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