How Can I Effectively Normalize The NDVI (Normalized Difference Vegetation Index) Values Derived From Sentinel-2 Imagery For A Specific Tropical Rainforest Region, Considering The High Variability In Sun Zenith Angles And Atmospheric Conditions During The Wet And Dry Seasons, While Also Accounting For The Bidirectional Reflectance Distribution Function (BRDF) Effects On The Observed Vegetation Reflectance?
To effectively normalize NDVI values from Sentinel-2 imagery for a tropical rainforest region, considering sun zenith angles, atmospheric conditions, and BRDF effects, follow this structured approach:
1. Atmospheric Correction
- Objective: Convert Top of Atmosphere (TOA) reflectance to Surface Reflectance.
- Tools: Use Sen2Cor or ATCOR for atmospheric correction. These tools account for atmospheric effects, providing more accurate surface reflectance values.
2. BRDF Correction
- Objective: Normalize reflectance for varying sun and sensor angles.
- Methods: Apply BRDF correction using models like Ross-Thick/Li-Sparse. Consider using the MODIS BRDF product as a reference for parameters, adapting them to Sentinel-2's higher resolution.
3. NDVI Calculation
- Process: Compute NDVI using the corrected surface reflectance from near-infrared and red bands.
4. Normalization Techniques
- Statistical Methods: Scale NDVI values to a specific range or use percentile-based normalization.
- Multi-Temporal Analysis: Use time-series data to account for seasonal variability, ensuring comparability across different conditions.
5. Additional Considerations
- Reference Areas: Consider using stable vegetation sites for normalization if feasible.
- Existing Studies: Review research papers or case studies for established workflows in tropical regions.
6. Implementation and Tools
- Software: Use tools like Sen2Cor for atmospheric correction. Explore additional software for BRDF correction if necessary.
- Pilot Testing: Test normalization techniques on a small area before large-scale application.
7. Further Research
- Guides and Tutorials: Consult resources on NDVI normalization, especially those addressing BRDF and atmospheric corrections, for optimal methods and algorithms.
By systematically addressing each factor—atmospheric conditions, BRDF effects, and seasonal variability—you can develop a robust normalization workflow tailored to your tropical rainforest study area.