Calibration and Validation of Polarimetric ALOS2-PALSAR2
Abstract
:1. Introduction
2. Lessons Learned from ALOS-PALSAR Calibration
- PALSAR2 CR measurements in the Amazonian rainforests, collected at free Faraday rotations [15], revealed insignificant return at HV and VH CR measurements. These CR measurements integrated in two different calibration methods led to the conclusion that ALOS-PALSAR is highly isolated with a cross-talk lower than −37 dB [5,6];
- The presence of small but still significant Faraday rotation (2–3°), at the JAXA (Japan), CCRS, DLR and, Chalmers U. calibration sites, induces a significant CR return at the cross-polarization (cross-pol) HV and VH. The integration of these contaminated CR response in the conventional polarimetric calibration methods [16,17,18] led to erroneous (i.e., biased) estimates of the antenna cross-talks.
3. The Extended Freeman-Van Zyl Calibration Method for Accurate Assessment of Antenna Cross-Talks
- Data symmetrization using the Freeman symmetrization method [17];
- Generation of the required calibration parameters and calibration using an extended version of van Zyl calibration method that leads to unbiased estimation of antenna X-talk for all azimuthally symmetric targets, including the ones with low HV return in comparison with HH, VV, and the HH-VV cross-correlation.
3.1. The FREEMAN Symmetrization Method
- Apply the van Zyl iterative process to derive and using an azimuthally symmetric target;
- Deduce F, , and using the additional information provided by a trihedral.
3.2. Reconsideration of Van Zyl Algorithm
3.3. Assessment of Antenna Cross-Talks Using an Iterative Method
Van Zyl’s Equations in Terms of for Azimuthally Symmetric Target
- Case 1: close to zero. The solutions are obtained by solving an analytical equation of 1st order. This analytical method is named Method 1;
- Case 2: of significant value (not negligible): In this case, an additional equation is needed to solve for the two unknowns. An iterative method similar to the one suggested by van Zyl can be applied to solve the problem.
- Derive and using Method 1, under the approximation that ;
- Compute the corresponding by inserting the two solutions and in Equation (5);
- If is close to zero or if is larger than the one computed in the previous iteration, or Test1 and Test2 are too low, stop the iterative process, and retain the solutions for and ;
- If not, update Equation (6) of with the actual value and apply Method 1 again with the new estimate;
- Repeat 1–3 until condition 4 is satisfied.
4. Assessment of PALSAR2 System Parameters at Low Faraday Rotation Conditions Using Amazonian Rainforests
4.1. Calibration Sites
4.2. Assessment of Polarimetric PALSAR2 Distortion Matrix
- and vary (slightly) with incidence angle, as might be expected. The magnitude of the ratio varies between 1.021 and 1.044; which corresponds to a variation in intensity ratio within 0.2 dB;
- Channel imbalance are very stable (in time) for the same mode, as can be noted for the 2 acquisitions in FP6-7 (last rows of Table 1);
- Channel imbalance phase varies with incidence angle, as might be expected. However, it remains stable (in time) for the same mode at different acquisitions, as can be noted for the two acquisitions in FP6-7.
4.3. Measurement of the Actual Faraday Rotation during PALSAR2 Acquisition
5. Impact of Significant Faraday Rotation on PALSAR2 Polarimetric Distortion Matrix Measurement
- The ratios of the cross-like polarization voltage, −20.03 dB and −19.95 dB do not correspond to the actual antenna cross-talk contamination of the cross-pol (HV and VH) by the like polarization (HH and VV), as could be misinterpreted if the Faraday rotation contamination is ignored ([7]). In fact, these cross-like polarization voltage ratios lead to an estimation of the Faraday rotation angle for a highly isolated antenna, as can be shown using Equation (15):Equation (16) is used to estimate the Faraday rotation during PALSAR2 acquisitions. The results obtained are similar (within 0.2) with the ones obtained with the Bickel and Bates method (Equation (11)); = 2.8° with , = 2.9° with in comparison with = 3.1° obtained over a forested area using Equation (11).
- The sum of the CR cross-pol voltages cancels the Faraday rotation contamination.This can be shown using the following equation derived from (15):Since the cross-talks are negligible, should be close to zero. Figure 9 presents the CR response of the averaged PALSAR2 image ()/2. The significant peaks that occur at HV and VH images of Figure 6 and Figure 7 vanish in Figure 9. At the HH and VV peak location, the intensity of the averaged cross-pol return vanishes in the CR surrounding clutter of radar backscattering (−18.23 dB) which is much lower than HH and VV retro-diffusion (about 15 dB).
6. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
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Mode | Date | CR Inc | ||||
---|---|---|---|---|---|---|
FP6-3 | 8−08 | 28 | 1.06 | −1.1 | 1.26 | −28.0 |
FP6-4 | 8−22 | 31 | 1.06 | −22.1 | 1.01 | −25.6 |
FP6-5 | 9−05 | 35 | 1.03 | −5.4 | 1.01 | −28.2 |
FP6-6 | 9−19 | 37 | 1.06 | −23.6 | 1.04 | −27.4 |
FP6-7 | 8−13 | 39 | 1.05 | −3.3 | 1.02 | −25.7 |
FP6-7 | 8−27 | 39 | 1.04 | −3.7 | 1.01 | −25.7 |
Mode | Date | |||
---|---|---|---|---|
FP6-3 | 8−08 | −40 | −45 | −0.12 |
FP6-4 | 8−22 | −44 | −41 | −0.19 |
FP6-5 | 9−05 | −41 | −41 | −0.24 |
FP6-6 | 9−19 | −45 | −42 | −0.15 |
FP6-7 | 8−13 | −40 | −40 | −0.17 |
FP6-7 | 8−27 | −40 | −44 | −0.16 |
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Touzi, R.; Shimada, M.; Motohka, T. Calibration and Validation of Polarimetric ALOS2-PALSAR2. Remote Sens. 2022, 14, 2452. https://doi.org/10.3390/rs14102452
Touzi R, Shimada M, Motohka T. Calibration and Validation of Polarimetric ALOS2-PALSAR2. Remote Sensing. 2022; 14(10):2452. https://doi.org/10.3390/rs14102452
Chicago/Turabian StyleTouzi, Ridha, Masanobu Shimada, and Takeshi Motohka. 2022. "Calibration and Validation of Polarimetric ALOS2-PALSAR2" Remote Sensing 14, no. 10: 2452. https://doi.org/10.3390/rs14102452
APA StyleTouzi, R., Shimada, M., & Motohka, T. (2022). Calibration and Validation of Polarimetric ALOS2-PALSAR2. Remote Sensing, 14(10), 2452. https://doi.org/10.3390/rs14102452