Deriving ocean color products using neural networks

被引:75
作者
Ioannou, Ioannis [1 ]
Gilerson, Alexander [1 ]
Gross, Barry [1 ]
Moshary, Fred [1 ]
Ahmed, Samir [1 ]
机构
[1] CUNY, Dept Elect Engn, Opt Remote Sensing Lab, New York, NY 10031 USA
关键词
Ocean color; Neural network; Inversion; MODIS; Absorption; Chlorophyll; CDOM; NAP; CHLOROPHYLL-A CONCENTRATION; SUSPENDED PARTICULATE MATTER; EASTERN ENGLISH-CHANNEL; OPTICAL-PROPERTIES; REMOTE ESTIMATION; TURBID WATERS; LAKE TAIHU; MODEL; PHYTOPLANKTON; VARIABILITY;
D O I
10.1016/j.rse.2013.02.015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper we develop a neural network (NN) algorithm for retrieving inherent optical properties (IOP) from above water remote sensing reflectances (Rrs) at available MODIS (or similar satellite) wavelengths. In previous work we used Hydrolight5 simulations of Rrs with widely varying globally representative constituent physical parameters as a training basis to develop a neural network algorithm, which, using the Rrs at the MODIS visible wavelengths (412, 443, 488, 531, 547 and 667 nm) as input, retrieves the in-water particulate backscattering (b(bp)), phytoplankton (a(ph)) and non-phytoplankton (a(dg)) absorption coefficients at 443 nm. In this work, using the same dataset, we develop a NN which takes these same Rrs as input, and produces an output which is used to separate the non-phytoplankton absorption coefficient (a(dg)) at 443 nm into dissolved (a(g)) and particulate (a(dm)) components. We then apply this synthetically trained algorithm to the NASA bio-Optical Marine Algorithm Data set (NOMAD) Rrs to retrieve IOP at 443 nm, with the measured NOMAD and retrieved IOP values showing good agreement. These retrieved MP along with their related Rrs values are then used to train an additional NN that produces chlorophyll concentration [Chl] as output. It is shown that these [Chl] values are retrieved more accurately when compared with ones retrieved with a similar approach which does not use IOP as input, as well as with those derived using the MODIS OC3 algorithm. (c) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:78 / 91
页数:14
相关论文
共 58 条
[1]  
[Anonymous], 2010, Light and Photosynthesis in Aquatic Ecosystems
[2]   Primary productivity in the Arctic Ocean: Impacts of complex optical properties and subsurface chlorophyll maxima on large-scale estimates [J].
Arrigo, Kevin R. ;
Matrai, Patricia A. ;
van Dijken, Gert L. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2011, 116
[3]  
Arst H, 2008, BOREAL ENVIRON RES, V13, P133
[4]   Influence of suspended particle concentration, composition and size on the variability of inherent optical properties of the Southern North Sea [J].
Astoreca, R. ;
Doxaran, D. ;
Ruddick, K. ;
Rousseau, V. ;
Lancelot, C. .
CONTINENTAL SHELF RESEARCH, 2012, 35 :117-128
[5]   HYPERBOLIC DISTRIBUTION OF PARTICLE SIZES [J].
BADER, H .
JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (15) :2822-+
[6]   Estimating suspended sediment concentrations from ocean colour measurements in moderately turbid waters; the impact of variable particle scattering properties [J].
Binding, CE ;
Bowers, DG ;
Mitchelson-Jacob, EG .
REMOTE SENSING OF ENVIRONMENT, 2005, 94 (03) :373-383
[7]   Particulate backscattering ratio at LEO 15 and its use to study particle composition and distribution [J].
Boss, E ;
Pegau, WS ;
Lee, M ;
Twardowski, M ;
Shybanov, E ;
Korotaev, G ;
Baratange, F .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2004, 109 (C1)
[8]   Shape of the particulate beam attenuation spectrum and its inversion to obtain the shape of the particulate size distribution [J].
Boss, E ;
Twardowski, MS ;
Herring, S .
APPLIED OPTICS, 2001, 40 (27) :4885-4893
[9]   A three-component model of phytoplankton size class for the Atlantic Ocean [J].
Brewin, Robert J. W. ;
Sathyendranath, Shubha ;
Hirata, Takafumi ;
Lavender, Samantha J. ;
Barciela, Rosa M. ;
Hardman-Mountford, Nick J. .
ECOLOGICAL MODELLING, 2010, 221 (11) :1472-1483
[10]   Modeling steady-state particle size spectra [J].
Burd, AB ;
Jackson, GA .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2002, 36 (03) :323-327