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卫星反演海洋固有光学特性的验证:提出的双色弹性后向散射激光雷达及反演理论

Validation of satellite-retrieved oceanic inherent optical properties: proposed two-color elastic backscatter lidar and retrieval theory.

作者信息

Hoge Frank E

机构信息

NASA Goddard Space Flight Center, Wallops Flight Facility, Building N-159, Wallops Island, Virginia 23337, USA.

出版信息

Appl Opt. 2003 Dec 20;42(36):7197-201. doi: 10.1364/ao.42.007197.

DOI:10.1364/ao.42.007197
PMID:14717299
Abstract

Recent radiative transfer models show that: (1) regardless of elastic lidar receiver field of view (FOV), at vanishing lidar depth the lidar-derived attenuation coefficient klidar --> a, where a is the total absorption coefficient per meter of depth; and (2) for a wide FOV as the lidar sensing depth approaches some large value (depending on water type), klidar --> Kd, where Kd is the diffuse attenuation for downwelling irradiance. As a result, it is shown that a time-resolved, dual-wavelength-laser, elastic-backscattering lidar can retrieve the three principal oceanic optical properties: (1) the absorption coefficient of phytoplankton aph, (2) the absorption coefficient of chromophoric dissolved organic matter (CDOM) aCDOM, and (3) the nonwater total constituent backscattering coefficient bbt. The lidar-retrieved aph, aCDOM, and bbt inherent optical properties can be used to validate corresponding satellite-derived products such as those from terra moderate-resolution imaging spectroradiometer (MODIS), Aqua MODIS, Sea-viewing Wide Field-of-view Sensor, (SeaWiFS), and other ocean color sensors.

摘要

最近的辐射传输模型表明

(1)无论弹性激光雷达接收器的视场(FOV)如何,在激光雷达深度趋近于零时,激光雷达得出的衰减系数klidar → a,其中a是每米深度的总吸收系数;(2)对于较宽的视场,当激光雷达探测深度接近某个较大值(取决于水体类型)时,klidar → Kd,其中Kd是下行辐照度的漫衰减。结果表明,一台时间分辨、双波长激光、弹性后向散射激光雷达能够反演三种主要的海洋光学特性:(1)浮游植物的吸收系数aph,(2)发色溶解有机物(CDOM)的吸收系数aCDOM,以及(3)非水体总成分后向散射系数bbt。激光雷达反演得到的aph、aCDOM和bbt等固有光学特性可用于验证相应的卫星衍生产品,如来自陆地中等分辨率成像光谱仪(MODIS)、水色卫星MODIS、宽视场海洋观测传感器(SeaWiFS)以及其他海洋颜色传感器的数据。

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