Abstract
A bio-optical dataset collected during the 1998–2007 period in the Yellow and East China Seas (YECS) was used to provide alternative empirical ocean-color algorithms in the retrieval of chlorophyll-a (Chl-a), total suspended matter (TSM), and colored dissolved organic matter (CDOM) absorption coefficients at 440 nm (ag440). Assuming that remote-sensing reflectance (Rrs) could be retrieved accurately, empirical algorithms for TChl (regionally tuned Tassan’s Chl-a algorithm) in case-1 waters (TChl2i in case-2 waters), TTSM (regionally tuned Tassan’s TSM algorithm), and Tag440 or Cag440 (regionally tuned Tassan’s or Carder’s ag440 algorithm) were able to retrieve Chl-a, TSM, and ag440 with uncertainties as high as 35, 46, and 35%, respectively. Applying the standard SeaWiFS Rrs, TChl was not viable in the eastern part of the YECS, which was associated with an inaccurate SeaWiFS Rrs retrieval because of improper atmospheric correction. TChl behaved better than other algorithms in the turbid case-2 waters, although overestimation was still observed. To retrieve more reliable Chl-a estimates with standard SeaWiFS Rrs in turbid water (a proxy for case-2 waters), we modified TChl for data with SeaWiFS normalized water-leaving radiance at 555 nm (nLw555) > 2 mW cm−2 μm−1 sr−1 (TChl2s). Finally, with standard SeaWiFS Rrs, we recommend switching algorithms from TChl2s (for case-2 waters) to MOCChl (SeaWiFS-modified NASA OC4v4 standard algorithm for case-1 waters) for retrieving Chl-a, which resulted in uncertainties as high as 49%. To retrieve TSM and ag440 using SeaWiFS Rrs, we recommend empirical algorithms for TTSM (pre-SeaWiFS-modified form) and MTag440 or MCag440 (SeaWiFS Rrs-modified forms of Tag440 or Cag440). These could retrieve with uncertainties as high as 82 and 52%, respectively.
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Abbreviations
- Chl-a :
-
Chlorophyll-a (mg m−3)
- TSM:
-
Total suspended matter (mg l−1)
- CDOM:
-
Colored dissolved organic matter
- ag440 :
-
CDOM absorption coefficient (m−1) at 440 nm
- Rrs:
-
Remote-sensing reflectance (sr−1)
- nLw:
-
Normalized water-leaving radiance (mW cm−2 μm−1 sr−1)
- TChl-O:
-
Original Tassan’s (1994) Chl-a algorithm
- TChl :
-
Regionally tuned Tassan’s (1994) Chl-a algorithm
- OC4v4:
-
NASA Chl-a standard algorithm
- OCChl :
-
Regionally tuned OC4v4
- TChl2i:
-
TChl optimized only for in situ nLw555 > 2 mW cm−2 μm−1 sr−1
- TChl_TChl2i:
-
Switching Chl-a algorithms: TChl for nLw555 ≤ 2 mW cm−2 μm−1 sr−1, TChl2i for nLw555 > 2 mW cm−2 μm−1 sr−1
- TTSM-O:
-
Original Tassan’s (1994) TSM algorithm
- TTSM :
-
Regionally tuned Tassan’s (1994) TSM algorithm
- CSeaTSM :
-
TSM algorithm implemented in SeaDAS (SeaWiFS Data Analysis System)
- CTSM :
-
Regionally tuned CSeaTSM
- Tag440-O:
-
Original Tassan’s (1994) ag440 algorithm
- Tag440 :
-
Regionally tuned Tassan’s (1994) ag440 algorithm
- Cag440 :
-
Regionally tuned Carder et al.’s (2003) ag440 algorithm
- MTChl :
-
Modified TChl based on standard SeaWiFS Rrs
- MOCChl :
-
Modified OCChl based on standard SeaWiFS Rrs
- TChl2 s:
-
Same as TChl2i except with standard SeaWiFS nLw555
- MOCChl_TChl2s:
-
Switched Chl-a algorithms: MOCChl for SeaWiFS nLw555 ≤ 2 mW cm−2 μm−1 sr−1, TChl2s for SeaWiFS nLw555 > 2 mW cm−2 μm−1 sr−1
- MTTSM :
-
Modified TTSM based on standard SeaWiFS Rrs
- MTag440 :
-
Modified Tag440 based on standard SeaWiFS Rrs
- MCag440 :
-
Modified Cag440 based on standard SeaWiFS Rrs
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Acknowledgments
This work was supported by the United Nations Development Programme (UNDP)/Global Environment Facility (GEF) Yellow Sea Large Marine Ecosystem (YSLME) Project. We would like to thank the SeaWiFS Project (code 970.2) and the Goddard Earth Sciences Data and Information Services Center/Distributed Active Archive Center (code 902) at the Goddard Space Flight Center, Greenbelt, MD, 20771, for the production and distribution of the SeaWiFS data, respectively.
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Siswanto, E., Tang, J., Yamaguchi, H. et al. Empirical ocean-color algorithms to retrieve chlorophyll-a, total suspended matter, and colored dissolved organic matter absorption coefficient in the Yellow and East China Seas. J Oceanogr 67, 627–650 (2011). https://doi.org/10.1007/s10872-011-0062-z
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DOI: https://doi.org/10.1007/s10872-011-0062-z