What Exactly is Launching?
NISAR (NASA–ISRO Synthetic Aperture Radar) is a joint Earth-observation satellite developed by NASA and ISRO. It features two SAR instruments on a single platform:
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NASA’s L-band SAR
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ISRO’s S-band SAR
It will orbit in a Sun-synchronous, dawn-dusk orbit at ~747 km altitude, 98.4° inclination, with a 12-day repeat cycle. A 12-meter gold-mesh reflector on a 9-meter boom captures a ~242 km swath. All data from NISAR will be free and openly available.
The satellite will be launched by India using the GSLV Mk-II (GSLV-F16) with a 4-meter fairing from the Satish Dhawan Space Centre (SDSC), Sriharikota. The lift-off mass is ~2,400 kg based on ISRO’s I-3K satellite bus.
Mission Duration:
NASA outlines a baseline 3-year science mission with consumables for ~5 years. As of July 25, 2025, ISRO officially lists the mission life as 5 years, aiming for extended operations.
Workshare Details:
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NASA: L-band radar, 12-m reflector, 9-m boom, GPS, solid-state recorder, high-rate telecom, payload data system
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ISRO: S-band radar, spacecraft (I-3K), GSLV Mk-II launch, satellite operations
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Both agencies will provide ground support and data distribution.
SAR Fundamentals (Static Core)
How SAR “Sees” (Active Microwave)
SAR is an active sensor: it sends microwave pulses and records echoes. It works day or night, in any weather, unlike passive optical sensors.
Synthetic Aperture: Instead of requiring a physically long antenna, SAR synthesizes one using the satellite’s motion to build high-resolution images.
Key Geometry Terms:
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Along-track (Azimuth): Direction of satellite motion
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Across-track (Range): Perpendicular to motion
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Slant range vs Ground range: Important SAR image dimensions
L-band vs S-band
Penetration and Use:
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L-band penetrates vegetation, dry soil, and snow, making it ideal for monitoring biomass, ground deformation, and ice sheets.
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S-band interacts more with leaves and surface textures, useful for assessing crop structure, moisture, and sea-ice characteristics.
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Dual-band SAR helps separate canopy and ground responses.
Polarimetry: NISAR supports various polarization modes (e.g., HH, HV, VH, VV). These enhance the ability to classify surfaces and estimate biomass.
Revisit and Repeat Cycles
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Repeat cycle: 12 days (same ground track)
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With both ascending and descending passes, average sampling = ~6 days
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Sun-synchronous orbit ensures the satellite crosses the same area at ~6 a.m. and ~6 p.m., maintaining consistent lighting — crucial for change detection.
Interferometry (InSAR)
SAR captures the phase of radar waves. Comparing the phase from two different passes gives line-of-sight displacement — down to millimetre accuracy.
Interferograms: These visualize movement (e.g., tectonic shifts) with color fringes, each corresponding to half the radar wavelength of displacement. L-band is better for vegetated terrains due to longer wavelength and better coherence.
Orbit & Mission Profile
Coverage Cadence: Entire Earth mapped every 12 days (ascending + descending = ~6-day average revisit).
Swath & Resolution:
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Swath: ~242 km
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Resolution: ~3–10 m (mode-dependent); ISRO cites 5–100 m
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Achieved via SweepSAR: Transmits over full swath and “sweeps” receiving beams for wide, high-res coverage.
What Can NISAR Measure?
Biomass & Carbon:
L-band penetrates canopy, enabling estimation of woody biomass, forest degradation, and carbon stock changes — useful for climate goals like REDD+.
Ground Deformation:
Tracks earthquakes, volcanic activity, subsidence, and landslides using InSAR — valuable for disaster risk reduction.
Cryosphere:
Monitors ice-sheet flow, glacier movement, and sea-ice — vital for understanding sea-level rise.
Coasts & Wetlands:
Maps shoreline changes, mangrove extent, storm impacts — works well even in cloudy monsoon regions.
Agriculture & Water:
Tracks crop extent, health, soil moisture, and impacts of irrigation or groundwater withdrawal.
Disaster Response:
Plans to provide data within hours during emergencies. NASA’s Alaska hub and ISRO will distribute these datasets rapidly.
ISRO–NASA Cooperation & Open Data
Both agencies follow a free and open data policy.
This policy enhances scientific use, supports operational agencies, and aligns with India’s evolving data policy.
Launch Vehicle Family: GSLV vs LVM3
The Launcher Chosen
GSLV Mk-II:
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Uses CE-7.5 cryogenic upper stage (LH₂/LOX, staged-combustion)
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Fairing options: 3.4 m (metallic), 4.0 m (ogive); NISAR uses 4.0 m
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Capacity: ~2.5 t to GTO, ~5 t to LEO
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NISAR (~2.4–2.8 t) fits within GSLV Mk-II’s range
Differences from LVM3
LVM3 (formerly GSLV Mk-III):
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Larger fairing: 5 m
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CE-20 engine (~200 kN) on C25 cryogenic stage
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Capacity: ~4 t to GTO, ~8 t to LEO
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Used for Chandrayaan-2/3, OneWeb, and Gaganyaan
Key Comparison:
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Engines: CE-7.5 (GSLV-II) vs CE-20 (LVM3)
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Fairing: 4 m vs 5 m
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Staging: GSLV Mk-II has three stages; LVM3 has two solid boosters, one liquid core, one cryo stage
Numbers at a Glance (Memorize for Exams)
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Orbit: 747 km altitude, 98.4° inclination, 12-day repeat, SSO 6 a.m./6 p.m.
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Antenna: 12 m reflector on 9 m boom
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Swath: ~242 km
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Resolution: 3–10 m typically, 5–100 m across modes
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Frequencies: L-band 1.257 GHz (~24 cm), S-band 3.2 GHz (~9 cm)
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Mission Duration: Baseline 3 years, goal 5 years
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Launcher: GSLV Mk-II with CE-7.5 engine, 4 m fairing
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Data Policy: Free and open via NASA and ISRO platforms
Likely UPSC Angles
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Benefits of dual-band SAR over single-band (L penetrates canopy, S captures fine surface structure)
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Concept of SweepSAR and how it resolves the swath–resolution trade-off
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Differences between Sun-synchronous vs Geostationary orbits for Earth observation
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Technical comparison between GSLV Mk-II and LVM3
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InSAR applications: subsidence, faults, volcanoes, glaciers
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Value of open data policy in supporting disaster management and scientific research