Classification of Inland Waters Based on Bio-Optical Properties

被引:22
|
作者
Shi, Kun [1 ,2 ]
Li, Yunmei [2 ]
Zhang, Yunlin [1 ]
Li, Lin [3 ]
Lv, Heng [2 ]
Song, Kaishan [4 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Taihu Lake Lab Ecosyst Stn, Nanjing 210008, Jiangsu, Peoples R China
[2] Nanjing Normal Univ, Coll Geog Sci, Minist Educ, Key Lab Virtual Geog Environm, Nanjing 210046, Jiangsu, Peoples R China
[3] Indiana Univ Purdue Univ, Dept Earth Sci, Indianapolis, IN 46202 USA
[4] Chinese Acad Sci, Northeast Inst Geog & Agr Ecol, Changchun 130012, Jilin, Peoples R China
基金
中国国家自然科学基金;
关键词
Cluster analysis; empirical orthogonal analysis; inland waters; remote sensing reflectance; scattering; Taihu Lake; CHLOROPHYLL-A CONCENTRATION; INHERENT OPTICAL-PROPERTIES; LIGHT-SCATTERING PROPERTIES; TURBID PRODUCTIVE WATERS; EASTERN ENGLISH-CHANNEL; OCEAN COLOR SPECTRA; ABSORPTION-SPECTRA; REMOTE ESTIMATION; BIOGEOCHEMICAL COMPOSITION; PHYTOPLANKTON ABSORPTION;
D O I
10.1109/JSTARS.2013.2290744
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
Multiple bio-optical measurements of optically active substances were conducted in Taihu Lake, Chaohu Lake, Three Gorges Reservoir, and Dianchi Lake (China). A hierarchical cluster analysis was applied to remote sensing spectra (R-rs(lambda)), by which those waters were clustered into three optically distinct types (Type I, Type II, and Type III). Absorption coefficients of phytoplankton were simulated using the linear function and the coefficients of the functions varied in different water types. The slope of colored dissolved organic matter (CDOM) absorption could be clustered into two classes, one class of high slope for Types I and II, whereas the other class of low slope for Type III. A uniform model was used for parameterization of the nonalgal particles absorption coefficients spectral between different water types. The power-law function was used to parameterize the scattering coefficient and the slope of scattering spectra could be classified into two groups of high slope for Types I and II, low slope for Type III. The composition of particles, particulate scattering, and nonalgal particulate absorption are the factors controlling the variability in R-rs(lambda) for corresponding type waters. Those results support such a fact that it is indispensable to classify waters before developing a model to estimate water quality parameters for multi-type optical waters.
引用
收藏
页码:543 / 561
页数:19
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