Validation of semi-analytical inversion models for inherent optical properties from ocean color in coastal Yellow Sea and East China Sea

The performances of three semi-analytical retrieval models for water inherent optical properties were validated in the coastal Yellow Sea and East China Sea, including the Quasi-Analytical Algorithm (QAA), the Garver-Siegel-Maritorena model (GSM) and the Over Constrained Linear Matrix (LM). The model-retrieved parameters, namely absorption coefficients of phytoplankton (aph), colored dissolved and detrital particulate matter (adg), total absorption coefficients (at), and backscattering coefficient of particles (bbp), were compared. The bio-optical datasets collected from a Yellow Sea and East China Sea cruise in April and September 2003 were used in the study. The QAA model performed the best in retrieval for all the coefficients, showing log-transformed root mean square errors of 0.306 for aph, 0.268 for adg, 0.144 for at, and 0.273 for bbp at 443 nm. The LM model showed a slightly larger deviation than the QAA model with a similar error trend for absorption coefficients, but it returned the largest uncertainties for bbp, with log-transformed root mean square error up to 0.646. The GSM model, however, yielded the largest and fluctuating errors along with wavelength for absorption coefficient retrievals. Substituting the fitting parameters from measured data for the empirical spectral parameters, all three models returned better results. These improvements demonstrated that semi-analytical algorithms designed for ocean water need regional modifications before applying to coastal areas. The QAA algorithm may be the most suitable model for retrieval for the Yellow Sea and East China Sea, and future model refinements should concentrate on regional modeling of inherent optical properties.

[1]  Stanford B. Hooker,et al.  Estimating absorption coefficients of colored dissolved organic matter (CDOM) using a semi-analytical algorithm for southern Beaufort Sea waters: application to deriving concentrations of dissolved organic carbon from space , 2012 .

[2]  T. Lin,et al.  The role of shelf mud depositional process and large river inputs on the fate of organochlorine pesticides in sediments of the Yellow and East China seas , 2011 .

[3]  M. Perry,et al.  Modeling in situ phytoplankton absorption from total absorption spectra in productive inland marine waters , 1989 .

[4]  Jinming Song,et al.  Phytoplankton distributions and their relationship with the environment in the Changjiang Estuary, China. , 2005, Marine pollution bulletin.

[5]  K. Carder,et al.  Absorption Spectrum of Phytoplankton Pigments Derived from Hyperspectral Remote-Sensing Reflectance , 2004 .

[6]  James W. Brown,et al.  A semianalytic radiance model of ocean color , 1988 .

[7]  E. Siswanto,et al.  Seasonal and spring interannual variations in satellite-observed chlorophyll-a in the Yellow and East China Seas: New datasets with reduced interference from high concentration of resuspended sediment , 2013 .

[8]  Giuseppe Zibordi,et al.  Assessment of satellite ocean color products at a coastal site , 2007 .

[9]  D. Siegel,et al.  An improved bio‐optical model for the remote sensing of Trichodesmium spp. blooms , 2005 .

[10]  Yi Ma,et al.  Satellite retrieval of inherent optical properties in the turbid waters of the Yellow Sea and the East China Sea , 2010 .

[11]  Priscila Goela,et al.  Specific absorption coefficient of phytoplankton off the Southwest coast of the Iberian Peninsula: A contribution to algorithm development for ocean colour remote sensing , 2013 .

[12]  M. Perry,et al.  In situ phytoplankton absorption, fluorescence emission, and particulate backscattering spectra determined from reflectance , 1995 .

[13]  K. Carder,et al.  Semianalytic Moderate‐Resolution Imaging Spectrometer algorithms for chlorophyll a and absorption with bio‐optical domains based on nitrate‐depletion temperatures , 1999 .

[14]  E. Fry,et al.  Absorption spectrum (380-700 nm) of pure water. II. Integrating cavity measurements. , 1997, Applied optics.

[15]  G. Ferrari,et al.  Geo-chemical and optical characterizations of suspended matter in European coastal waters , 2003 .

[16]  P. V. Nagamani,et al.  Comparison of Inherent Optical Properties (IOPs) in Open and Coastal Waters of Arabian Sea Using In-Situ Bio-Optical Data , 2011 .

[17]  R. Arnone,et al.  Deriving inherent optical properties from water color: a multiband quasi-analytical algorithm for optically deep waters. , 2002, Applied optics.

[18]  J. Kindle,et al.  Euphotic zone depth: Its derivation and implication to ocean-color remote sensing , 2007 .

[19]  Sang-Woo Kim,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 , 2011 .

[20]  Dennis A. Hansell,et al.  Global distribution and dynamics of colored dissolved and detrital organic materials , 2002 .

[21]  A. Morel Optical properties of pure water and pure sea water , 1974 .

[22]  S. Doney,et al.  Impact of phytoplankton community size on a linked global ocean optical and ecosystem model , 2012 .

[23]  Tang Junwu,et al.  A research on statistical retrieval algorithms and spectral characteristics of the total absorption coefficients in the Yellow Sea and the East China Sea , 2006 .

[24]  Norman J. McCormick,et al.  Inherent optical property estimation in deep waters. , 2011, Optics express.

[25]  Deyong Sun,et al.  Validation of a Quasi-Analytical Algorithm for Highly Turbid Eutrophic Water of Meiliang Bay in Taihu Lake, China , 2009, IEEE Transactions on Geoscience and Remote Sensing.

[26]  Frank E. Hoge,et al.  An analysis of model and radiance measurement errors , 1996 .

[27]  John Marra,et al.  Phytoplankton pigment absorption: A strong predictor of primary productivity in the surface ocean , 2007 .

[28]  S. Maritorena,et al.  An Evaluation of Oceanographic Radiometers and Deployment Methodologies , 2000 .

[29]  Stéphane Maritorena,et al.  Optimization of a semianalytical ocean color model for global-scale applications. , 2002, Applied optics.

[30]  Palanisamy Shanmugam,et al.  An evaluation of inversion models for retrieval of inherent optical properties from ocean color in coastal and open sea waters around Korea , 2010 .

[31]  D. Siegel,et al.  Inherent optical property inversion of ocean color spectra and its biogeochemical interpretation: 1. Time series from the Sargasso Sea , 1997 .

[32]  Menghua Wang,et al.  Remote Sensing of Inherent Optical Properties : Fundamentals , 2009 .

[33]  S. Thiria,et al.  Retrieval of pigment concentrations and size structure of algal populations from their absorption spectra using multilayered perceptrons. , 2007, Applied optics.

[34]  Daji Huang,et al.  Sea-surface temperature fronts in the Yellow and East China Seas from TRMM microwave imager data , 2010 .

[35]  Janet W. Campbell,et al.  The lognormal distribution as a model for bio‐optical variability in the sea , 1995 .

[36]  Junwu Tang,et al.  Backscattering ratio variation and its implications for studying particle composition: A case study in Yellow and East China seas , 2010 .

[37]  TANGJunwu,et al.  The statistic inversion algorithms of water constituents for the Huanghai Sea and the East China Sea , 2004 .

[38]  Minwei Zhang,et al.  Retrieval of total suspended matter concentration in the Yellow and East China Seas from MODIS imagery , 2010 .

[39]  Song Qing,et al.  Retrieval of inherent optical properties of the Yellow Sea and East China Sea using a quasi-analytical algorithm , 2011 .

[40]  Song Qingjun,et al.  The study on the scattering properties in the Huanghai Sea and East China Sea , 2006 .

[41]  Lee Zhong-ping An evaluation of two semi-analytical ocean color algorithms for waters of the South China Sea , 2009 .

[42]  A. Morel Optical modeling of the upper ocean in relation to its biogenous matter content (case I waters) , 1988 .