Mapping particulate organic carbon in lakes across China using OLCI/ Sentinel-3 imagery

被引:6
作者
Liu, Dong [1 ,2 ]
Yu, Shujie [3 ]
Wilson, Harriet [2 ]
Shi, Kun [4 ]
Qi, Tianci [1 ]
Luo, Wenlei [4 ,5 ]
Duan, Mengwei [1 ]
Qiu, Zhiqiang [1 ]
Duan, Hongtao [1 ,6 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Key Lab Watershed Geog Sci, Nanjing 210008, Peoples R China
[2] Univ Stirling, Sch Biol & Environm Sci, Stirling FK9 4LA, Scotland
[3] Minist Nat Resources, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Peoples R China
[4] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Taihu Lab Lake Ecosyst Res, State Key Lab Lake Sci & Environm, Nanjing 210008, Peoples R China
[5] Fuxianhu Stn Plateau Deep Lake Field Sci Observat, Yuxi 653100, Yunnan, Peoples R China
[6] Univ Chinese Acad Sci Nanjing UCASNJ, Nanjing 211135, Peoples R China
关键词
Particulate organic carbon; Bio-optical properties; Inland lakes; Remote sensing; OLCI/Sentinel-3; imagery; TO-CHLOROPHYLL RATIO; INLAND; OCEAN; ABSORPTION; POC; PHYTOPLANKTON; REFLECTANCE; EMISSIONS; DYNAMICS; GROWTH;
D O I
10.1016/j.watres.2023.121034
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Remote sensing monitoring of particulate organic carbon (POC) concentration is essential for understanding phytoplankton productivity, carbon storage, and water quality in global lakes. Some algorithms have been proposed, but only for regional eutrophic lakes. Based on in-situ data (N = 1269) in 49 lakes across China, we developed a blended POC algorithm by distinguishing Type-I and Type-II waters. Compared to Type-I, Type-II waters had higher reflectance peak around 560 nm (>0.0125 sr(-1)) and mean POC (4.65 +/- 4.11 vs. 2.66 +/- 3.37 mg/L). Furthermore, because POC was highly related to algal production (r = 0.85), a three-band index (R-2 = 0.65) and the phytoplankton fluorescence peak height (R-2 = 0.63) were adopted to estimate POC in Type-I and Type-II waters, respectively. The novel algorithm got a mean absolute percent difference (MAPD) of 35.93 % and outperformed three state-of-the-art formulas with MAPD values of 40.56-76.42 %. Then, the novel algorithm was applied to OLCI/Sentinel-3 imagery, and we first obtained a national map of POC in 450 Chinese lakes (> 20 km(2)), which presented an apparent spatial pattern of "low in the west and high in the east". In brief, water classification should be considered when remotely monitoring lake POC concentration over a large area. Moreover, a process-oriented method is required when calculating water column POC storage from satellite-derived POC concentrations in type-II waters. Our results contribute substantially to advancing the dynamic observation of the lake carbon cycle using satellite data.
引用
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页数:14
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