4.7 Article

Radiometric Cross-Calibration of Tiangong-2 MWI Visible/NIR Channels over Aquatic Environments using MODIS

期刊

REMOTE SENSING
卷 10, 期 11, 页码 -

出版社

MDPI
DOI: 10.3390/rs10111803

关键词

atmospheric correction; cross calibration; open oceans; total suspended matter; inland water

资金

  1. National Key R&D Program of China [2018YFB0504900, 2018YFB0504904, 2016YFCO200900]
  2. National Natural Science Foundation of China [41571344, 41701379, 41331174, 41071261, 40906092, 40971193, 41101415, 41401388, 41206169, 41406205]
  3. China Postdoctoral Science Foundation
  4. program of Key Laboratory for National Geographic Census and Monitoring
  5. National Administration of Surveying, Mapping and Geoinformation [2014NGCM]
  6. Natural Science Foundation of Jiangxi, China [20161BAB213074]
  7. Wuhan University Luojia Talented Young Scholar project [32442]
  8. LIESMARS Special Research Funding
  9. High Resolution Earth Observation Systems of National Science and Technology Major Projects [41-Y20A31-9003-15/17]
  10. 985 Project of Wuhan University

向作者/读者索取更多资源

The Moderate-Resolution Wide-Wavelength Imager (MWI), onboard the Tiangong-2 (TG-2) Space Lab, is an experimental satellite sensor designed for the next-generation Chinese ocean color satellites. The MWI imagery is not sufficiently radiometrically calibrated, and therefore, the cross-calibration is urgently needed to provide high quality ocean color products for MWI observations. We proposed a simple and effective cross-calibration scheme for MWI data using well calibrated Moderate Resolution Imaging Spectroradiometer (MODIS) imagery over aquatic environments. The path radiance of the MWI was estimated using the quasi-synchronized MODIS images as well as the MODIS Rayleigh and aerosol look up tables (LUTs) from SeaWiFS Data Analysis System 7.4 (SeaDAS 7.4). The results showed that the coefficients of determination (R-2) of the calibration coefficients were larger than 0.97, with sufficient matched areas to perform cross-calibration for MWI. Compared with the simulated Top of Atmosphere (TOA) radiance using synchronized MODIS images, all errors calculated with the calibration coefficients retrieved in this paper were less than 5.2%, and lower than the lab calibrated coefficients. The Rayleigh-corrected reflectance (rho(rc)), remote sensing reflectance (R-rs) and total suspended matter (TSM) products of MWI, MODIS and the Geostationary Ocean Color Imager (GOCI) images for Taihu Lake in China were compared. The distribution of rho(rc) of MWI, MODIS and GOCI agreed well, except for band 667 nm of MODIS, which might have been saturated in relatively turbid waters. Besides, the R-rs used to retrieve TSM among MWI, MODIS and GOCI was also consistent. The root mean square errors (RMSE), mean biases (MB) and mean ratios (MR) between MWI R-rs and MODIS R-rs (or GOCI R-rs) were less than 0.20 sr(-1), 5.52% and within 1 +/- 0.023, respectively. In addition, the derived TSM from MWI and GOCI also agreed with a R-2 of 0.90, MB of 13.75%, MR of 0.97 and RMSE of 9.43 mg/L. Cross-calibration coefficients retrieved in this paper will contribute to quantitative applications of MWI. This method can be extended easily to other similar ocean color satellite missions.

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