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基于GOCI影像的太湖水体漫衰减系数遥感反演
摘要点击 1528  全文点击 1161  投稿时间:2015-01-20  修订日期:2015-05-20
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中文关键词  遥感  漫衰减系数  反演模型  GOCI影像  太湖
英文关键词  remote sensing  diffuse attenuation coefficient  retrieval mode  GOCI images  Lake Taihu
作者单位E-mail
王珊珊 江苏省地理信息资源开发与利用协同创新中心, 南京 210023
南京师范大学地理科学学院, 南京 210023 
wshanshan1110@163.com 
李云梅 江苏省地理信息资源开发与利用协同创新中心, 南京 210023
南京师范大学地理科学学院, 南京 210023
南京师范大学江苏省碳氮循环过程与污染控制重点实验室, 南京 210023 
yunmei2009@gmail.com 
王桥 环境保护部卫星环境应用中心, 北京 100029  
吕恒 江苏省地理信息资源开发与利用协同创新中心, 南京 210023
南京师范大学地理科学学院, 南京 210023 
 
中文摘要
      漫衰减系数是水体光学中的一个重要参数. 采用2006~2009年的太湖野外实测数据,分析了太湖水体漫衰减系数光谱特性及其影响因子,在此基础上,结合GOCI传感器数据,分别构建漫衰减系数经验模型和半分析模型,寻找适合GOCI影像的太湖漫衰减系数反演模型,并分析太湖水体漫衰减系数的时空变化特征. 结果表明: 1太湖水体漫衰减系数主要受非色素颗粒物吸收主导,以GOCI第4、5、7波段构建的多元线性模型反演漫衰减系数,效果最好;2太湖水体漫衰减系数值域主要分布在0~15 m-1,大体可以分为3个等级,低值区: 0~4 m-1,中值区: 4~8 m-1,高值区: 8~15 m-1,部分高值区高于15 m-1;3太湖水体漫衰减系数存在一定时空差异性,从空间上来说,太湖水体漫衰减系数呈现一定的梯度性,从东部到西部逐渐变高;从时间上来说,早上太湖漫衰减系数相对较高,从上午到下午,大体上呈现逐渐降低的趋势.
英文摘要
      Diffuse attenuation coefficient (Kd) is an important parameter in water body optics.The spectral characteristics of Kd in Lake Taihu and its impact factors were analyzed using the in situ measured data from 2006-2009.Then, empirical models and semi-analysis models were built based on the GOCI data to estimate Kd, in order to find a suitable retrieval model for GOCI and analyze the spatial and temporal variations of diffuse attenuation coefficient in Lake Taihu.The result indicates that: ① The main impact factor of diffuse attenuation coefficient at 490 nm is the non-algal particles absorption coefficient, and the combination model with GOCI bands 4, 5 and 7, namely the near infrared band, the red band and the green band, has the highest precision for the inversion of Kd(490);② the range of Kd of Lake Taihu distributes between 0 to 15 m-1, and that can be divided into three levels generally, i.e., the range of the low value between 0-4 m-1, the range of the medium value between 4-8 m-1, and the range of the high value between 8-15 m-1.While, occasionally, some values are higher than 15 m-1;③ the Kd of Lake Taihu distributes with notable spatial and temporal difference.At the view of spatial distribution, the Kd values get higher from the east to the west of Lake Taihu;from the perspective of time, the Kd is relatively high in the morning and then shows a tendency of gradually reduce with the time.

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