Acta Optica Sinica, Volume. 45, Issue 12, 1228009(2025)
Dependence of Aerosol Satellite Remote Sensing Polarization and Multi-Angle Indicators Based on Forward-Inverse Simulation
Fig. 1. Flowchart of top-of-atmosphere reflectance simulation and GRASP inversion of AOD
Fig. 2. Particle size distributions of five types of aerosols involved in simulation. (a) Particle size distributions of five coappearance models of fine and coarse particles; (b)‒(f) particle size distributions of fine and coarse models corresponding to five models
Fig. 3. Line charts of evaluation indicators of AOD inversion results varying with number of polarization channels. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 4. When the number of polarization channels is 1, line charts of evaluation indicators of AOD inversion results varying with polarization band. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 5. When the number of polarization channels is 2, line charts of evaluation indicators of AOD inversion results varying with polarization band. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 6. When the number of polarization channels is 3, line charts of evaluation indicators of AOD inversion results varying with polarization bands. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 7. When the number of polarization channels is 4, line charts of evaluation indicators of AOD inversion results varying with polarization bands. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 8. When the number of polarization channels is 5, line charts of evaluation indicators of AOD inversion results varying with polarization bands. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
Fig. 9. Consistency verification of AOD inversion results with different numbers of observation angles
Fig. 10. Line charts of AOD inversion results varying with number of observation angle. (a) Pearson correlation coefficient; (b) root mean square error; (c) mean absolute error; (d) proportion of points within expected error range
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Yanfeng Li, Han Wang, Yueran Sun, Wenzhe Dong. Dependence of Aerosol Satellite Remote Sensing Polarization and Multi-Angle Indicators Based on Forward-Inverse Simulation[J]. Acta Optica Sinica, 2025, 45(12): 1228009
Category: Remote Sensing and Sensors
Received: Nov. 28, 2024
Accepted: Jan. 22, 2025
Published Online: Jun. 23, 2025
The Author Email: Han Wang (ms.h.wang@cumt.edu.cn)
CSTR:32393.14.AOS241885