共 2 条
Synergistic detection of chlorophyll-a concentration vertical profile by spaceborne lidar ICESat-2 and passive optical observations
被引:0
|作者:
Zhang, Xuechun
[1
,2
,3
]
Ma, Yi
[2
,3
]
Li, Zhongwei
[1
]
Zhang, Jingyu
[2
,3
]
机构:
[1] China Univ Petr East China, Coll Oceanog & Space Informat, Qingdao 266500, Peoples R China
[2] Minist Nat Resources, Inst Oceanog 1, Lab Marine Phys & Remote Sensing, Qingdao 266061, Peoples R China
[3] Minist Nat Resources, Technol Innovat Ctr Ocean Telemetry, Qingdao 266061, Peoples R China
基金:
中国国家自然科学基金;
关键词:
ICESat-2 spaceborne lidar;
Passive remote sensing;
Chlorophyll-a;
Diffuse attenuation coefficient;
Ocean Color;
OCEAN COLOR SENSORS;
BACKSCATTERING;
WATERS;
UNCERTAINTIES;
SUBSURFACE;
RETRIEVAL;
DEEP;
D O I:
10.1016/j.jag.2024.104035
中图分类号:
TP7 [遥感技术];
学科分类号:
081102 ;
0816 ;
081602 ;
083002 ;
1404 ;
摘要:
The tremendous improvement for satellite remote sensing has provided mankind with the feasibility of observing large-scale ocean phenomena from space. Passive remote sensing of ocean color has delivered continuous records of ocean surface information, although there are inherent limitations to this natural light-dependent measurement. The development of spaceborne lidars breaks through the restrictions of passive techniques that are unavailable for obtaining the vertical characteristics of water column, and provides a new approach to the detection of ocean subsurface. In this study, the active spaceborne lidar ICESat-2 and passive optical satellite are fused, to establish an inversion method of lidar equation and semi-analytical model. The diffuse attenuation coefficient ( k d ) was estimated in various areas of the global oceans, and vertical profiles of chlorophyll-a concentration ( Chla ) were further obtained. The results showed that Mean Absolute Errors (MAE) of Chla derived by the proposed method with BGC-Argo data were in the range of 0.003 -0.14 mg/m 3 , and the Mean Absolute Percentage Error (MAPE) was between 12.5 % and 26.9 %; Comparison with ocean color products indicated that R 2 of Chla was in the range of 0.84 -0.98, and MAE of k d was in the range of 0.004 -0.021 m-1 . The multiple validation approaches have demonstrated the effectiveness of water column profile detection with ICESat-2 lidar and passive satellite, which contributes to the enhanced understanding of ocean subsurface phytoplankton and their spatial or temporal variations.
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