- Overview
- Project Objective
- Study Area
- Data Selection Strategy
- Data Source & Acquisition
- Image Selection Criteria
- Required Software
- Methodology
- Workflow Summary
- Results
- Challenges Encountered
- Reproducibility Notes
- Tools Used
- Future Improvements
- References
This project demonstrates the generation of a Digital Elevation Model (DEM) from Sentinel-1 Synthetic Aperture Radar (SAR) imagery using Interferometric SAR (InSAR) processing techniques in ESA SNAP.
By exploiting phase differences between two SAR acquisitions, terrain elevation was reconstructed for the Delamar Mountain Wilderness, Nevada, USA.
To generate an accurate, terrain-corrected DEM from Sentinel-1 SLC imagery through interferometric processing and phase unwrapping while minimizing coherence loss and atmospheric distortions.
Nevada was selected due to its favorable environmental conditions for InSAR processing:
- Arid desert climate
- Sparse vegetation cover
- Minimal surface water bodies
- Low relative humidity (~30–38%)
These conditions improve interferometric coherence and reduce atmospheric interference.
| Feature | Description |
|---|---|
| Elevation Range | 790 – 1800 ft |
| Topography | Deep winding canyons |
| Landforms | Rocky peaks & steep cliffs |
| Slope Features | Long sloping bajadas |
DEM generation using InSAR requires:
- Stable surface reflectivity between acquisitions
- Minimal vegetation-induced decorrelation
- Low atmospheric moisture
To reduce atmospheric distortion, imagery was selected from Nevada’s dry season:
May – September
- May
- August
SAR imagery was obtained from the Copernicus Programme.
| Parameter | Value |
|---|---|
| Satellite | Sentinel-1 |
| Product Type | SLC (Single Look Complex) |
| Acquisition Mode | IW (Interferometric Wide Swath) |
| Download Portal | Copernicus Data Hub |
Additional image IDs and study boundaries are available in the
helplist.txtfile.
To ensure reliable interferometric DEM generation:
Both images must:
- Be acquired in Ascending orbit
- Maintain identical viewing geometry
To ensure sufficient topographic sensitivity:
- Perpendicular Baseline > 150 m
- ASF Vertex
| Software | Purpose |
|---|---|
| ESA SNAP | InSAR Processing |
| SNAPHU | Phase Unwrapping |
| Google Earth Pro | DEM Visualization |
- Update and install SNAP plugins
- Reinstall SNAPHU after output path modification
- Import Sentinel-1 SLC scenes
-
Apply S-1 TOPS Split
- Select subswath
- Select polarization
- Select burst covering AOI
-
Apply Precise Orbit File
- Perform S-1 Back Geocoding
- Apply Enhanced Spectral Diversity
- Perform Interferogram Formation
- Run TOPS Deburst
- Apply Goldstein Phase Filtering
- Perform Multilooking
- Range = 5
- Azimuth = 1
-
Export to SNAPHU with:
- Cost Mode = TOPO
- Row Overlap = 300
- Column Overlap = 300
- Tiling = 4×4
-
Run SNAPHU Unwrapping
-
Import unwrapped output back into SNAP
- Perform Phase to Elevation
- Save DEM output
- Perform Terrain Correction
- Export final DEM as KMZ
Import Data
↓
TOPS Split
↓
Apply Orbit File
↓
Back Geocoding
↓
Enhanced Spectral Diversity
↓
Interferogram Formation
↓
TOPS Deburst
↓
Goldstein Filtering
↓
Multilooking
↓
SNAPHU Export
↓
SNAPHU Unwrapping
↓
Phase to Elevation
↓
Terrain Correction
↓
Export DEM
SNAPHU phase unwrapping was computationally expensive.
- Used 4×4 tiling during SNAPHU export.
- Introduced minor bounding line artifacts in the unwrapped interferogram.
To reproduce this workflow accurately:
- Use Sentinel-1 SLC IW imagery only
- Maintain same orbit direction for image pair
- Ensure baseline > 150 m
- Select dry-season acquisitions
- Preserve all listed SNAP/SNAPHU parameters
- Maintain identical filtering/multilooking settings
Potential enhancements to improve DEM quality:
- Experiment with alternative filtering techniques
- Test different baseline thresholds
- Compare results using varied SNAPHU tiling configurations
- Integrate Ground Control Points (GCPs) for validation
- Quantitatively assess DEM accuracy using RMSE
