Radar & SAR

Sentinel-1 and radar imagery: backscatter, polarisation, speckle, terrain geometry, floods and change through cloud.

A radar pulse reflecting away from calm water, scattering off a field and bouncing back from a building corner. brightness is roughness, not colourcalm water · −20 dBfield · −10 dBbuildings · −4 dBSentinel-1 carries its own illumination, so cloud, night and storms do not stop it

Radar is the one sensor on this site that makes its own light. Sentinel-1 sends 5.5 cm microwaves sideways at the ground and records what comes back, which means it works at night, through cloud, and during exactly the storms that optical satellites miss. That is why flood maps, ship detection and winter crop monitoring are radar work.

The cost is that a radar image is not a photograph of anything. Brightness is roughness, moisture and how the surface faces the sensor — water is black, cities are white, and every pixel carries speckle, a grain that is not noise but interference. Values arrive as linear power with a nodata flag of −32768, averages taken in decibels come out wrong, mountains lean towards the sensor, and two passes from different tracks disagree about a slope that never changed.

The concepts below settle what backscatter is, what VV and VH each see, where speckle comes from and what terrain does to the geometry; the how-to guides find, read, filter, composite and difference real Sentinel-1 scenes; and the fixes are the four ways the numbers come out wrong — noisy, negative, misaligned, or showing water where there is none.

Learning paths run through this topic too — see the end of this page.

🧭 Start with the concepts

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⚙️ Then do the task

Step-by-step walkthroughs with code you can copy and adapt.

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🔧 When it breaks

The errors this topic produces, with the cause explained rather than just the command.

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