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OCEAN LIDAR MEASUREMENTS OF BEAM ATTENUATION AND A ROADMAPTO ACCURATE PHYTOPLANKTON BIOMASS ESTIMATES

机译:梁衰减的海洋激光乐队测量和路边浮游植物的浮游植物生物量估计

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Beam attenuation coefficient, c, provides an important optical index of plankton standing stocks, such as phytoplankton biomass and total particulate carbon concentration. Unfortunately, c has proven difficult to quantify through remote sensing. Here, we introduce an innovative approach for estimating c using lidar depolarization measurements and diffuse attenuation coefficients from ocean color products or lidar measurements of Brillouin scattering. The new approach is based on a theoretical formula established from Monte Carlo simulations that links the depolarization ratio of sea water to the ratio of diffuse attenuation Kd and beam attenuation C (i.e., a multiple scattering factor). On July 17, 2014, the CALIPSO satellite was tilted 30° off-nadir for one nighttime orbit in order to minimize ocean surface backscatter and demonstrate the lidar ocean subsurface measurement concept from space. Depolarization ratios of ocean subsurface backscatter are measured accurately. Beam attenuation coefficients computed from the depolarization ratio measurements compare well with empirical estimates from ocean color measurements. We further verify the beam attenuation coefficient retrievals using aircraft-based high spectral resolution lidar (HSRL) data that are collocated with in-water optical measurements.
机译:光束衰减系数C为浮游生物股票提供了重要的光学指标,例如Phytoplankton生物量和总颗粒碳浓度。不幸的是,C已经证明难以通过遥感量量化。在这里,我们介绍了一种使用LiDAR去极化测量和来自海洋颜色产品的漫射衰减系数来估计C的创新方法,或者是Brillouin散射的LIDAR测量。新方法基于从蒙特卡罗模拟建立的理论公式,该蒙特卡罗模拟将海水的去极化比与漫射衰减Kd和光束衰减比的比率联系起来(即,多散射因子)。 2014年7月17日,Calipso卫星为一个夜晚轨道倾斜了30°Off-Nadir,以最大限度地减少海洋表面反向散射并展示Lidar海洋地下测量概念。海洋地下反向散射的去极化比是准确测量的。从去极化比率测量计算的光束衰减系数与海洋颜色测量的经验估计相比很好。我们进一步使用与水中光学测量的飞机的高光谱分辨率LIIDAR(HSRL)数据验证光束衰减系数检索。

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