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HY-1 CCD宽波段水色要素反演算法

马超飞 蒋兴伟 唐军武 王晓梅 李铜基 黄海军 任敬萍

马超飞, 蒋兴伟, 唐军武, 王晓梅, 李铜基, 黄海军, 任敬萍. HY-1 CCD宽波段水色要素反演算法[J]. 海洋学报, 2005, 27(4): 38-44.
引用本文: 马超飞, 蒋兴伟, 唐军武, 王晓梅, 李铜基, 黄海军, 任敬萍. HY-1 CCD宽波段水色要素反演算法[J]. 海洋学报, 2005, 27(4): 38-44.
MA Chao-fei, JIANG Xing-wei, TANG Jun-wu, WANG Xiao-mei, LI Tong-ji, HUANG Hai-jun, REN Jing-ping. Inverse algorithms of ocean constituents for HY-1/CCD broadband data[J]. Haiyang Xuebao, 2005, 27(4): 38-44.
Citation: MA Chao-fei, JIANG Xing-wei, TANG Jun-wu, WANG Xiao-mei, LI Tong-ji, HUANG Hai-jun, REN Jing-ping. Inverse algorithms of ocean constituents for HY-1/CCD broadband data[J]. Haiyang Xuebao, 2005, 27(4): 38-44.

HY-1 CCD宽波段水色要素反演算法

基金项目: 国家“863”高技术计划资助项目(2002AA639160,2001AA636010);国家“十五”攻关资助项目(2001BA603B06)

Inverse algorithms of ocean constituents for HY-1/CCD broadband data

  • 摘要: 利用2003年春季黄海、东海区现场实测数据,建立了HY1卫星4波段CCD成像仪水色要素反演算法.由于HY1CCD的宽波段特性阻碍了黄色物质的反演,因此反演的水色要素仅包括水体表层的总悬浮物、悬浮泥沙(SS)以及叶绿素a的浓度.现场遥感反射率光谱由ASD地物波谱仪测量,对于叶绿素a的浓度利用现场萃取荧光法测量,总悬浮物、悬浮泥沙由实验室滤膜称重法获得.反演算法的拟合相关系数均大于0.88,平均相对误差在40%以下.对反演算法进行了误差灵敏度分析,结果表明对于总悬浮物、悬浮泥沙和低浊度水体中的叶绿素a的浓度反演算法能够满足日常的业务运行要求,但是对于高浊度水体中叶绿素a的浓度反演算法对某个波段组合比较敏感,仍需要进一步探讨.
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出版历程
  • 收稿日期:  2004-02-16
  • 修回日期:  2004-10-18

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