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Atmospheric correction of SeaWiFS imagery for turbid coastal and inland waters
作者姓名:HE Xianqiang  PAN Delu  MAO Zhihua
作者单位:KeyLaboratoryofOceanDynamicProcessesandSatelliteOceanographyofStateOceanicAdministration,Hangzhou310012,China//SecondInstituteofOceanography,StateOceanicAdministration,Hangzhou310012,China
基金项目:国家高技术研究发展计划(863计划),Thank the National Satellite Ocean Application Service (NSOAS) for providing the in-situ data
摘    要:A practical algorithm of atmospheric correction for turbid coastal and inland waters is provided. The present algorithm uses the property that the water-leaving radiance at 412 nm increases very tittle with the increasing of water turbidity. Thus, in very turbid coastal and inland waters, the radiance at 412 nm can be used to estimate the aerosol scattering radiance at 865 nm. The performance of the new algorithm is validated with simulation for several cases. It is found that the retrieved remotely sensed reflectance is usually with error less than 10% for the first six bands of SeaWiFS. This new algorithm is also tested under various atmospheric conditions in the Changjiang River Estuary and the Hangzhou Bay where the sediment concentration is very high and the standard SeaWiFS atmospheric correction algorithm creates a mask due to atmospheric correction failure. The result proves the efficiency of this simple algorithm in reducing the errors of the water-leaving radiance retrieving using SeaWiFS satellite data.

关 键 词:大气修正  海洋水质  海岸混浊  WiFS算法  浮质散射辐射率
收稿时间:2004/1/11 0:00:00
修稿时间:2004/6/20 0:00:00

Atmospheric correction of SeaWiFS imagery for turbid coastal and inland waters
HE Xianqiang,PAN Delu,MAO Zhihua.Atmospheric correction of SeaWiFS imagery for turbid coastal and inland waters[J].Acta Oceanologica Sinica,2004,23(4):609-615.
Authors:HE Xianqiang  PAN Delu and MAO Zhihua
Institution:1. Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography of State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Shanghai Institute of Technical Physics, Ch
2. Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography of State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
Abstract:A practical algorithm of atmospheric correction for turbid coastal and inland waters is provided. The presentalgorithm uses the property that the water-leaving radiance at 412 nm increases very little with the increasing of waterturbidity. Thus, in very turbid coastal and inland waters, the radiance at 412 nm can be used to estimate the aerosolscattering radiance at 865 nm. The performance of the new algorithm is validated with simulation for several cases. Itis found that the retrieved remotely sensed reflectance is usually with error less than 10% for the first six bands ofSeaWiFS. This new algorithm is also tested under various atmospheric conditions in the Changjiang River Estuaryand the Hangzhou Bay where the sediment concentration is very high and the standard SeaWiFS atmosphericcorrection algorithm creates a mask due to atmospheric correction failure. The result proves the efficiency of thissimple algorithm in reducing the errors of the water-leaving radiance retrieving using SeaWiFS satellite data.
Keywords:atmospheric correction  SeaWiFS  Case II waters
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