Comparative Analysis of GOCI Ocean Color Products

The Geostationary Ocean Color Imager (GOCI) is the first geostationary ocean color sensor in orbit that provides bio-optical properties from coastal and open waters around the Korean Peninsula at unprecedented temporal resolution. In this study, we compare the normalized water-leaving radiance (nLw)...

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Main Authors: Ruhul Amin, Mark David Lewis, Adam Lawson, Richard W. Gould Jr., Paul Martinolich, Rong-Rong Li, Sherwin Ladner, Sonia Gallegos
Format: Article
Language:English
Published: MDPI AG 2015-10-01
Series:Sensors
Subjects:
Online Access:http://www.mdpi.com/1424-8220/15/10/25703
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author Ruhul Amin
Mark David Lewis
Adam Lawson
Richard W. Gould Jr.
Paul Martinolich
Rong-Rong Li
Sherwin Ladner
Sonia Gallegos
author_facet Ruhul Amin
Mark David Lewis
Adam Lawson
Richard W. Gould Jr.
Paul Martinolich
Rong-Rong Li
Sherwin Ladner
Sonia Gallegos
author_sort Ruhul Amin
collection DOAJ
description The Geostationary Ocean Color Imager (GOCI) is the first geostationary ocean color sensor in orbit that provides bio-optical properties from coastal and open waters around the Korean Peninsula at unprecedented temporal resolution. In this study, we compare the normalized water-leaving radiance (nLw) products generated by the Naval Research Laboratory Automated Processing System (APS) with those produced by the stand-alone software package, the GOCI Data Processing System (GDPS), developed by the Korean Ocean Research & Development Institute (KORDI). Both results are then compared to the nLw measured by the above water radiometer at the Ieodo site. This above-water radiometer is part of the Aerosol Robotic NETwork (AeroNET). The results indicate that the APS and GDPS processed  correlates well within the same image slot where the coefficient of determination (r2) is higher than 0.84 for all the bands from 412 nm to 745 nm. The agreement between APS and the AeroNET data is higher when compared to the GDPS results. The Root-Mean-Squared-Error (RMSE) between AeroNET and APS data ranges from 0.24 [mW/(cm2srμm)] at 555 nm to 0.52 [mW/(cm2srμm)]  at 412 nm while RMSE between AeroNET and GDPS data ranges from 0.47 [mW/(cm2srμm)] at 443 nm to 0.69 [mW/(cm2srμm)]  at 490 nm.
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spelling doaj.art-fea084a93b9d443a918929f42c3baf282022-12-22T04:22:05ZengMDPI AGSensors1424-82202015-10-011510257032571510.3390/s151025703s151025703Comparative Analysis of GOCI Ocean Color ProductsRuhul Amin0Mark David Lewis1Adam Lawson2Richard W. Gould Jr.3Paul Martinolich4Rong-Rong Li5Sherwin Ladner6Sonia Gallegos7BioOptoSense LLC, New Orleans, LA 70115, USANaval Research Laboratory, Code 7331, Stennis Space Center, MS 39529, USANaval Research Laboratory, Code 7331, Stennis Space Center, MS 39529, USANaval Research Laboratory, Code 7331, Stennis Space Center, MS 39529, USAVencore, Inc., Stennis Space Center, MS 39529, USANaval Research Laboratory, Code 7231, Building 2, Washington, DC 20375, USANaval Research Laboratory, Code 7331, Stennis Space Center, MS 39529, USANaval Research Laboratory, Code 7331, Stennis Space Center, MS 39529, USAThe Geostationary Ocean Color Imager (GOCI) is the first geostationary ocean color sensor in orbit that provides bio-optical properties from coastal and open waters around the Korean Peninsula at unprecedented temporal resolution. In this study, we compare the normalized water-leaving radiance (nLw) products generated by the Naval Research Laboratory Automated Processing System (APS) with those produced by the stand-alone software package, the GOCI Data Processing System (GDPS), developed by the Korean Ocean Research & Development Institute (KORDI). Both results are then compared to the nLw measured by the above water radiometer at the Ieodo site. This above-water radiometer is part of the Aerosol Robotic NETwork (AeroNET). The results indicate that the APS and GDPS processed  correlates well within the same image slot where the coefficient of determination (r2) is higher than 0.84 for all the bands from 412 nm to 745 nm. The agreement between APS and the AeroNET data is higher when compared to the GDPS results. The Root-Mean-Squared-Error (RMSE) between AeroNET and APS data ranges from 0.24 [mW/(cm2srμm)] at 555 nm to 0.52 [mW/(cm2srμm)]  at 412 nm while RMSE between AeroNET and GDPS data ranges from 0.47 [mW/(cm2srμm)] at 443 nm to 0.69 [mW/(cm2srμm)]  at 490 nm.http://www.mdpi.com/1424-8220/15/10/25703geostationary satelliteocean color remote sensingbio-optical productsAPSGDPS
spellingShingle Ruhul Amin
Mark David Lewis
Adam Lawson
Richard W. Gould Jr.
Paul Martinolich
Rong-Rong Li
Sherwin Ladner
Sonia Gallegos
Comparative Analysis of GOCI Ocean Color Products
Sensors
geostationary satellite
ocean color remote sensing
bio-optical products
APS
GDPS
title Comparative Analysis of GOCI Ocean Color Products
title_full Comparative Analysis of GOCI Ocean Color Products
title_fullStr Comparative Analysis of GOCI Ocean Color Products
title_full_unstemmed Comparative Analysis of GOCI Ocean Color Products
title_short Comparative Analysis of GOCI Ocean Color Products
title_sort comparative analysis of goci ocean color products
topic geostationary satellite
ocean color remote sensing
bio-optical products
APS
GDPS
url http://www.mdpi.com/1424-8220/15/10/25703
work_keys_str_mv AT ruhulamin comparativeanalysisofgocioceancolorproducts
AT markdavidlewis comparativeanalysisofgocioceancolorproducts
AT adamlawson comparativeanalysisofgocioceancolorproducts
AT richardwgouldjr comparativeanalysisofgocioceancolorproducts
AT paulmartinolich comparativeanalysisofgocioceancolorproducts
AT rongrongli comparativeanalysisofgocioceancolorproducts
AT sherwinladner comparativeanalysisofgocioceancolorproducts
AT soniagallegos comparativeanalysisofgocioceancolorproducts