A neural network model for remote sensing of diffuse attenuation coefficient in global oceanic and coastal waters: Exemplifying the applicability of the model to the coastal regions in Eastern China Seas

被引:29
作者
Chen, Jun [1 ,2 ]
Cui, Tingwei [3 ]
Ishizaka, Joji [4 ]
Lin, Changsong [1 ]
机构
[1] China Univ Geosci, Sch Ocean Sci, Beijing 100083, Peoples R China
[2] Qingdao Inst Marine Geol, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China
[3] State Ocean Adm, Inst Oceanog 1, Qingdao 266071, Peoples R China
[4] Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
基金
中国国家自然科学基金;
关键词
Remote sensing; Global oceanic and coastal waters; Neural network; Diffuse attenuation coefficient; DOWNWELLING IRRADIANCE; TRANSPORT PROCESSES; COLOR PRODUCTS; FINE SEDIMENT; CASE-1; WATERS; CHLOROPHYLL-A; BOHAI SEA; REFLECTANCE; VALIDATION; RETRIEVAL;
D O I
10.1016/j.rse.2014.02.019
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
global oceanic and coastal waters, a multilayer back propagation neural network (MBPNN) is developed to retrieve the diffuse attenuation coefficient for the downwelling spectral irradiance at the wavelength 490 nm (K-d(490)). The applicability of Lee's quasi-analytical algorithm-based semi-analytical model, Wang's switching model, Chen's semi-analytical model, jamet's neural network model, and the MBPNN model is evaluated using the NASA bio-optical marine algorithm dataset (NOMAD) and the Eastern China Seas dataset. Based on the comparison of Kd(490) predicted by these five models, with field measurements taken in global oceanic and coastal waters, it is found that the MBPNN model provides a stronger performance than the Lee, Wang, Chen, and Jamet's models. The atmospheric effects on the MODIS data are eliminated using near-infrared band-based and shortwave infrared band-based combined models, and the K-d(490) is quantified from the MODIS data after atmospheric correction using the MBPNN model. The study results indicate that the MBPNN model produces similar to 28% uncertainty in estimating K-d(490) from the MODIS data. Finally, an exemplification of the applicability of the model to the coastal regions in the Eastern China Seas is carried out. Our results suggest that the K-d(490) shows a large variation in the Eastern China Seas, ranging from 0.02 to 4.0 m(-1), with an average value of -0.17 m(-1). (C) 2014 Elsevier Inc. All rights reserved.
引用
收藏
页码:168 / 177
页数:10
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