Yuan Dapeng, Chen Peng, Mao Zhihua, Zhang Xianliang, Zhang Zhenhua, Xie Congshuang, Zhong Chunyi, Qian Zheng
Appl Opt. 2021 Dec 20;60(36):11180-11188. doi: 10.1364/AO.442647.
The potential of Brillouin scattering lidar for detecting the mixed layer depth (MLD) was studied. We simulated the Brillouin scattering lidar signal in various water environmental parameters and developed an MLD retrieval model for Brillouin scattering lidar data. We first analyzed the theoretical maximum detectable depth for Brillouin scattering lidar in low-latitude sea regions based on the multiple scattering lidar equations. Subsequently, a theoretical method for calculating the Brillouin scattering frequency shift and linewidth was derived based on the international thermodynamic equation of seawater-2010 and the coupled wave equations. Then we used the theoretical method and the temperature-salinity (T-S) profile of the global Argo data in low-latitude regions to simulate the vertical profile distribution of the Brillouin scattering frequency shift and linewidth. Furthermore, we used a maximum angle method to estimate the ocean MLD in low-latitude regions based on the vertical profile distribution of the Brillouin scattering frequency shift and density in seawater. They are well correlated, which indicates that the frequency-shift component of the Brillouin scattering lidar signal for estimating ocean MLD is feasible and reliable. It appears that airborne or spaceborne Brillouin scattering lidar technology provides great potential for high-efficiency, large-area, and long-term monitoring of the global ocean MLD and upper-ocean water bodies.
研究了布里渊散射激光雷达探测混合层深度(MLD)的潜力。我们在各种水环境参数下模拟了布里渊散射激光雷达信号,并开发了一种用于布里渊散射激光雷达数据的MLD反演模型。我们首先基于多次散射激光雷达方程分析了低纬度海域布里渊散射激光雷达的理论最大可探测深度。随后,基于国际海水热力学方程-2010和耦合波动方程推导了计算布里渊散射频移和线宽的理论方法。然后,我们利用该理论方法和低纬度地区全球Argo数据的温度-盐度(T-S)剖面,模拟了布里渊散射频移和线宽的垂直剖面分布。此外,我们基于布里渊散射频移和海水密度的垂直剖面分布,采用最大角度法估算了低纬度地区的海洋MLD。它们具有良好的相关性,这表明用于估算海洋MLD的布里渊散射激光雷达信号的频移分量是可行和可靠的。机载或星载布里渊散射激光雷达技术似乎为全球海洋MLD和上层水体的高效、大面积和长期监测提供了巨大潜力。