FN Archimer Export Format
PT J
TI System vicarious calibration of GCOM-C/SGLI visible and near-infrared channels
BT 
AF Murakami, Hiroshi
   Antoine, David
   Vellucci, Vincenzo
   Frouin, Robert
AS 1:1;2:2,3;3:3;4:4;
FF 1:;2:;3:;4:;
C1 Earth Observation Research Center, Japan Aerospace Exploration Agency, 2-1-1 Sengen, Tsukuba, Ibaraki, 305-8505, Japan
   Remote Sensing and Satellite Research Group, School of Earth and Planetary Sciences, Curtin University, Perth, WA, 6845, Australia
   Sorbonne Université, CNRS Institut de la Mer de Villefranche, IMEV, 06230, Villefranche-sur-Mer, France
   Scripps Institution of Oceanography, University of California San Diego, 9500 Gilman Drive, La Jolla, CA, 92093-0224, USA
C2 JAXA, JAPAN
   UNIV CURTIN, AUSTRALIA
   UNIV SORBONNE, FRANCE
   UNIV CALIF SAN DIEGO, USA
IF 2.3
TC 5
UR https://archimer.ifremer.fr/doc/00750/86246/91545.pdf
LA English
DT Article
CR BOUSSOLE
DE ;GCOM-C;SHIKISAI;SGLI;Remote sensing;Ocean color;Calibration
AB Vicarious calibration coefficients (kv) of Second-generation GLobal Imager (SGLI) for ocean color processing were derived using in-situ radiometric buoy measurements from the Marine Optical BuoY (MOBY) and the BOUée pour l'acquiSition d'une Série Optique à Long termE (BOUSSOLE). Two aerosol-model look up tables (LUTs) used in the GCOM-C aerosol retrieval algorithm (LUT-A) and in the previous version of ocean color atmospheric correction algorithm (LUT-B) were tested in the procedures to calculate kv and retrieve remote sensing reflectance (Rrs) and aerosol optical thickness (AOT). Bias of the processed Rrs compared to AERONET-OC Rrs was reduced by applying the determined kv (i.e., corrected SGLI radiance = original SGLI radiance/kv). LUT-A yielded smaller AOT bias compared to AERONET-OC AOT; on the other hand, LUT-B gave smaller Rrs noise due to gentle slope of the aerosol reflectance even though it caused AOT overestimation. When kv was derived by adjusting to the AOT measurements, kv was about 1.1 by LUT-A and 1.2 by LUT-B in the near-infrared (NIR) channel. However, the kv in the NIR channel was close to 1.0 when AOT and land surface reflectance measurements of Radiometric Calibration Network (RadCalNet) were used. The LUT-A with kv from MOBY and BOUSSOLE are currently adopted for the SGLI standard ocean color processing. Improvement is needed, however, to design an optimal LUT suitable for both aerosol and ocean color purposes. 
PY 2022
PD AUG
SO Journal Of Oceanography
SN 0916-8370
PU Springer Science and Business Media LLC
VL 78
IS 4
UT 000751598600001
BP 245
EP 261
DI 10.1007/s10872-022-00632-x
ID 86246
ER

EF