Remote sensing estimation of colored dissolved organic matter (CDOM) in optically shallow waters

被引:45
作者
Li, Jiwei [1 ]
Yu, Qian [1 ]
Tian, Yong Q. [2 ,3 ]
Becker, Brian L. [2 ,3 ]
机构
[1] Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA
[2] Cent Michigan Univ, Inst Great Lakes Res, Mt Pleasant, MI 48859 USA
[3] Cent Michigan Univ, Dept Geog, Mt Pleasant, MI 48859 USA
基金
美国国家科学基金会;
关键词
CDOM; Carbon cycle; Optically shallow waters; Land-water interface; SBOP; Bottom effect index; Adaptive estimation approach; QUASI-ANALYTICAL ALGORITHM; FLORIDA-KEYS WATERS; ABSORPTION-COEFFICIENTS; DIFFUSE ATTENUATION; HYPERION IMAGERY; MATRIX-INVERSION; COASTAL WATERS; INLAND WATERS; IN-SITU; CARBON;
D O I
10.1016/j.isprsjprs.2017.03.015
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
It is not well understood how bottom reflectance of optically shallow waters affects the algorithm performance of colored dissolved organic matters (CDOM) retrieval. This study proposes a new algorithm that considers bottom reflectance in estimating CDOM absorption from optically shallow inland or coastal waters. The field sampling was conducted during four research cruises within the Saginaw River, Kawkawlin River and Saginaw Bay of Lake Huron. A stratified field sampling campaign collected water samples, determined the depth at each sampling location and measured optical properties. The sampled CDOM absorption at 440 nm broadly ranged from 0.12 to 8.46 m(-1). Field sample analysis revealed that bottom reflectance does significantly change water apparent optical properties. We developed a CDOM retrieval algorithm (Shallow water Bio-Optical Properties algorithm, SBOP) that effectively reduces uncertainty by considering bottom reflectance in shallow waters. By incorporating the bottom contribution in upwelling radiances, the SBOP algorithm was able to explain 74% of the variance of CDOM values (RMSE = 0.22 and R-2 = 0.74). The bottom effect index (BEI) was introduced to efficiently separate optically shallow and optically deep waters. Based on the BEI, an adaptive approach was proposed that references the amount of bottom effect in order to identify the most suitable algorithm (optically shallow water algorithm [SBOP] or optically deep water algorithm [QAA-CDOM]) to improve CDOM estimation (RMSE = 0.22 and R-2 = 0.81). Our results potentially help to advance the capability of remote sensing in monitoring carbon pools at the land-water interface. (C) 2017 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:98 / 110
页数:13
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