Quantitative Analysis of Chlorophyll-a Reflectance Spectrum in Red Spectral Region of Water
Ma Wan-dong1,2,3; Xing Qian-guo1,4; Zhang Yuan-zhi5; Shi Ping1; Liu Ya-long1
发表期刊SPECTROSCOPY AND SPECTRAL ANALYSIS
ISSN1000-0593
2010-02-01
卷号30期号:2页码:313-317
关键词Chlorophyll-a Reflectance Spectrum Reflectance Peak In Red Spectral Region Fluorescence Peak Spectrum Simulation
产权排序[Ma Wan-dong; Xing Qian-guo; Shi Ping; Liu Ya-long] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China; [Ma Wan-dong] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China; [Ma Wan-dong] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China; [Xing Qian-guo] CNRS, UMR 8187, LOG, F-62930 Wimereux, France; [Zhang Yuan-zhi] Chinese Univ Hong Kong, Inst Space & Earth Informat Sci, Hong Kong, Hong Kong, Peoples R China
通讯作者Xing, QG, Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
作者部门信息集成与应用实验室 
英文摘要The chlorophyll-a concentration in waters is one of the main parameters of water color remote sensing in case 11 waters. There is a reflectance peak in red band region because of inherent optical properties. Based on the coefficients of absorption and backscattering of waters, colored dissolved organic matter (CDOM), tripton and chlorophyll-a, the reflectance of remote sensing was simulated according to the forward radiation transfer model without the consideration of fluorescence peak. The reflectance peak intensity and reflectance peak position at different wavelengths in red band region were analyzed with different chlorophyll-a concentration. There is a good linear relationship between the red reflectance peak intensity and chlorophyll-a concentration when the chlorophyll-a concentration is 1-50 mu g . L-1. But the linear relationship between the reflectance peak intensity and chlorophyll-a concentration will decrease with the increasing chlorophyll-a concentration. When chlorophyll-a concentration is up to 1 000 mu g . L-1, the logarithm relationship between the reflectance peak intensity and chlorophyll-a concentration is better than linear relationship. The wavelength position of reflectance peak in red band region will shift towards larger wavelength at logarithmic growth rate with increasing chlorophyll-a concentration, and the logarithm relationship will be more apparent with the increasing chlorophyll-a concentration. The same trend happens to the reflectance peak intensity and the wavelength position of peak in red region with different in-water constituents, such as CDOM, tripton and so on. Furthermore, according to the comparison with fluorescence peak, the authors also found that the reflectance peak intensity and the wavelength position of peak in red region are different from those of the fluorescence peak.; The chlorophyll-a concentration in waters is one of the main parameters of water color remote sensing in case 11 waters. There is a reflectance peak in red band region because of inherent optical properties. Based on the coefficients of absorption and backscattering of waters, colored dissolved organic matter (CDOM), tripton and chlorophyll-a, the reflectance of remote sensing was simulated according to the forward radiation transfer model without the consideration of fluorescence peak. The reflectance peak intensity and reflectance peak position at different wavelengths in red band region were analyzed with different chlorophyll-a concentration. There is a good linear relationship between the red reflectance peak intensity and chlorophyll-a concentration when the chlorophyll-a concentration is 1-50 mu g . L(-1). But the linear relationship between the reflectance peak intensity and chlorophyll-a concentration will decrease with the increasing chlorophyll-a concentration. When chlorophyll-a concentration is up to 1 000 mu g . L(-1), the logarithm relationship between the reflectance peak intensity and chlorophyll-a concentration is better than linear relationship. The wavelength position of reflectance peak in red band region will shift towards larger wavelength at logarithmic growth rate with increasing chlorophyll-a concentration, and the logarithm relationship will be more apparent with the increasing chlorophyll-a concentration. The same trend happens to the reflectance peak intensity and the wavelength position of peak in red region with different in-water constituents, such as CDOM, tripton and so on. Furthermore, according to the comparison with fluorescence peak, the authors also found that the reflectance peak intensity and the wavelength position of peak in red region are different from those of the fluorescence peak.
文章类型Article
收录类别SCI
语种英语
关键词[WOS]APPARENT OPTICAL-PROPERTIES ; OCEAN COLOR ; TIME-SERIES ; ALGORITHM ; INHERENT ; SEAWIFS ; FLUORESCENCE ; MODEL
研究领域[WOS]Spectroscopy
WOS记录号WOS:000274321800007
引用统计
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/3813
专题中国科学院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心
作者单位1.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
3.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
4.CNRS, UMR 8187, LOG, F-62930 Wimereux, France
5.Chinese Univ Hong Kong, Inst Space & Earth Informat Sci, Hong Kong, Hong Kong, Peoples R China
推荐引用方式
GB/T 7714
Ma Wan-dong,Xing Qian-guo,Zhang Yuan-zhi,et al. Quantitative Analysis of Chlorophyll-a Reflectance Spectrum in Red Spectral Region of Water[J]. SPECTROSCOPY AND SPECTRAL ANALYSIS,2010,30(2):313-317.
APA Ma Wan-dong,Xing Qian-guo,Zhang Yuan-zhi,Shi Ping,&Liu Ya-long.(2010).Quantitative Analysis of Chlorophyll-a Reflectance Spectrum in Red Spectral Region of Water.SPECTROSCOPY AND SPECTRAL ANALYSIS,30(2),313-317.
MLA Ma Wan-dong,et al."Quantitative Analysis of Chlorophyll-a Reflectance Spectrum in Red Spectral Region of Water".SPECTROSCOPY AND SPECTRAL ANALYSIS 30.2(2010):313-317.
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