Fusion of Sun-Synchronous and Geostationary Images for Coastal and Ocean Color Survey Application to OLCI (Sentinel-3) and FCI (MTG)

Open ocean and coastal area monitoring requires multispectral satellite images with a middle spatial resolution (~300 m) and a high temporal repeatability (~1 h). As no current satellite sensors have such features, the aim of this study is to propose a fusion method to merge images delivered by a low earth orbit (LEO) sensor with images delivered by a geostationary earth orbit (GEO) sensor. This fusion method, called spatial spectral temporal fusion (SSTF), is applied to the future sensors- Ocean and Land Color Instrument (OLCI) (on Sentinel-3) and Flexible Combined Imager (FCI) (on Meteosat Third Generation) whose images were simulated. The OLCI bands, acquired at t0, are divided by the oversampled corresponding FCI band acquired at t0 and multiplied by the FCI bands acquired at t1. The fusion product is used for the next fusion at t1 and so on. The high temporal resolution of FCI allows its signal-to-noise ratio (SNR) to be enhanced by the means of temporal filtering. The fusion quality indicator ERGAS computed between SSTF fusion products and reference images is around 0.75, once the FCI images are filtered from the noise and 1.08 before filtering. We also compared the estimation of chlorophyll (Chl), suspended particulate matter (SPM), and colored dissolved organic matter (CDOM) maps from the fusion products with the input simulation maps. The comparison shows an average relative errors on Chl, SPM, and CDOM, respectively, of 64.6%, 6.2%, and 9.5% with the SSTF method. The SSTF method was also compared with an existing fusion method called the spatial and temporal adaptive reflectance fusion model (STARFM).

[1]  C. Mobley,et al.  Hyperspectral remote sensing for shallow waters. I. A semianalytical model. , 1998, Applied optics.

[2]  Pierre Gouton,et al.  Simulation of Future Geostationary Ocean Color Images , 2012, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[3]  Dariusz Stramski,et al.  Variations in the light absorption coefficients of phytoplankton, nonalgal particles, and dissolved organic matter in coastal waters around Europe , 2003 .

[4]  C. Mobley Light and Water: Radiative Transfer in Natural Waters , 1994 .

[5]  Fabrice Ardhuin,et al.  Sediment transport in the Bay of Marseille : Role of extrem events. , 2013 .

[6]  B. Nechad,et al.  Optical remote sensing of coastal waters from geostationary platforms: a feasibility study - Mapping Total Suspended Matter with SEVIRI , 2008 .

[7]  Naoto Yokoya,et al.  Hyperspectral, multispectral, and panchromatic data fusion based on coupled non-negative matrix factorization , 2011, 2011 3rd Workshop on Hyperspectral Image and Signal Processing: Evolution in Remote Sensing (WHISPERS).

[8]  R. W. Austin,et al.  Nimbus-7 Coastal Zone Color Scanner: System Description and Initial Imagery , 1980, Science.

[9]  Vincent Faure,et al.  Investigation and sensitivity analysis of a mechanistic phytoplankton model implemented in a new modular numerical tool (Eco3M) dedicated to biogeochemical modelling , 2006 .

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

[11]  Quinten Vanhellemont,et al.  Synergy between polar-orbiting and geostationary sensors: Remote sensing of the ocean at high spatial and high temporal resolution☆ , 2014 .

[12]  Quinten Vanhellemont,et al.  Challenges and opportunities for geostationary ocean colour remote sensing of regional seas: A review of recent results , 2014 .

[13]  Emmanuel Boss,et al.  Theoretical derivation of the depth average of remotely sensed optical parameters. , 2005, Optics express.

[14]  Audrey Minghelli-Roman,et al.  Fusion of Multispectral Images by Extension of the Pan-Sharpening ARSIS Method , 2014, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[15]  F. Dumas,et al.  An external–internal mode coupling for a 3D hydrodynamical model for applications at regional scale (MARS) , 2008 .

[16]  Luciano Alparone,et al.  Image fusion—the ARSIS concept and some successful implementation schemes , 2003 .

[17]  G. Zibordi,et al.  Assessment of MERIS ocean color data products for European seas , 2013 .

[18]  B. Berruti,et al.  Ocean and Land Color Imager on Sentinel‐3 , 2015 .

[19]  Menghua Wang,et al.  Evaluation of the VIIRS Ocean Color Monitoring Performance in Coastal Regions , 2013 .

[20]  Mathew R. Schwaller,et al.  On the blending of the Landsat and MODIS surface reflectance: predicting daily Landsat surface reflectance , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[21]  H. Gordon,et al.  Remote sensing optical properties of a stratified ocean: an improved interpretation. , 1980, Applied optics.

[22]  Audrey Minghelli-Roman,et al.  Spatial resolution improvement by merging MERIS-ETM images for coastal water monitoring , 2006, IEEE Geoscience and Remote Sensing Letters.

[23]  Dieter Oertel,et al.  Unmixing-based multisensor multiresolution image fusion , 1999, IEEE Trans. Geosci. Remote. Sens..

[24]  Dariusz Stramski,et al.  Light scattering properties of marine particles in coastal and open ocean waters as related to the particle mass concentration , 2003 .

[25]  Peter J. Minnett,et al.  An overview of MODIS capabilities for ocean science observations , 1998, IEEE Trans. Geosci. Remote. Sens..

[26]  Audrey Minghelli-Roman,et al.  Spatial resolution improvement of MeRIS images by fusion with TM images , 2001, IEEE Trans. Geosci. Remote. Sens..

[27]  Paolo Lazzari,et al.  Development of a 3D Coupled Physical-Biogeochemical Model for the Marseille Coastal Area (NW Mediterranean Sea): What Complexity Is Required in the Coastal Zone? , 2013, PloS one.

[28]  W. Verhoef,et al.  Simulation of hyperspectral and directional radiance images using coupled biophysical and atmospheric radiative transfer models , 2003 .

[29]  I. Pairaud,et al.  Hydrology and circulation in a coastal area off Marseille: Validation of a nested 3D model with observations , 2011 .

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

[31]  Lucien Wald,et al.  Quality of high resolution synthesised images: Is there a simple criterion ? , 2000 .

[32]  F. Gohin,et al.  A five channel chlorophyll concentration algorithm applied to SeaWiFS data processed by SeaDAS in coastal waters , 2002 .

[33]  Jong-Kuk Choi,et al.  GOCI, the world's first geostationary ocean color observation satellite, for the monitoring of temporal variability in coastal water turbidity , 2012 .

[34]  Michael Unser,et al.  B-spline signal processing. I. Theory , 1993, IEEE Trans. Signal Process..

[35]  Kevin Ruddick,et al.  Diurnal variability of turbidity and light attenuation in the southern North Sea from the SEVIRI geostationary sensor , 2012 .

[36]  D. C. Robertson,et al.  MODTRAN cloud and multiple scattering upgrades with application to AVIRIS , 1998 .

[37]  R. Keys Cubic convolution interpolation for digital image processing , 1981 .

[38]  Hoepffner Nicolas,et al.  Why Ocean Colour? The Societal Benefits of Ocean-Colour Technology , 2008 .

[39]  Ivane Pairaud,et al.  Intrusion of Rhone River diluted water into the Bay of Marseille: Generation processes and impacts on ecosystem functioning , 2014 .

[40]  W. Esaias,et al.  SeaWiFS technical report series. Volume 1: An overview of SeaWiFS and ocean color , 1992 .

[41]  Edward H. Adelson,et al.  The Laplacian Pyramid as a Compact Image Code , 1983, IEEE Trans. Commun..