Working & Applications

Working

Synthetic aperture radar (SAR) refers to a technique for producing fine-resolution images from a resolution-limited radar system. It requires that the radar be moving in a straight line, either on an airplane or,rocket. The basic principle of any imaging radar is to emit an electromagnetic signal (which travels at the speed of light) toward a surface and record the amount of signal that bounces/echoes back, or “backscatters,” and it's time delay.

The SAR works similar to a phased array, but contrary to a large number of the parallel antenna elements of a phased array, SAR uses one antenna in time-multiplex. The different geometric positions of the antenna elements are the result of the moving platform now.

The wavelengths that remote sensing radars use to observe Earth’s surface are microwaves, typically in the range of a few to tens of centimetres. Because the radar signal loses energy as it travels – at a rate equivalent to the beam width (wavelength / antenna size) – by the time it hits the surface, the beam has spread dramatically. For example, with a signal wavelength of 10 centimeters and an antenna of 10 meters in diameter, the beam width is 1/100 radians (0.6 degrees).

From an altitude of 1,000 kilometers, the resulting beam width on the ground becomes a very large 10 km, producing an image resolution which is insufficient for most applications. SAR is the solution to this dilemma as it can vastly improve the resolution.

SAR techniques take advantage of the fact that the radar is moving in orbit to synthesize a virtual 10-km-long antenna from the physical 10-m antenna in the direction of flight. As the radar moves along its path, it sweeps the antenna’s footprint across the ground while continuously transmitting pulses – short signal bursts separated by time – and receiving the echoes of the returned pulses.

As a target (like a ship) first enters the radar beam, the backscattered echoes from each transmitted pulse begin to be recorded. As the platform continues to move forward, all echoes from the target for each pulse are recorded during the entire time that the target is within the beam. The point at which the target leaves the view of the radar beam some time later, determines the length of the simulated or synthesized antenna. The synthesized expanding beamwidth, combined with the increased time a target is within the beam as ground range increases, balances each other, such that the resolution remains constant across the entire swath.

The SAR-processor stores all the radar returned signals, as amplitudes and phases, for the time period T from position A to D. Now it is possible to reconstruct the signal which would have been obtained by an antenna of length v · T, where v is the platform speed. As the line of sight direction changes along the radar platform trajectory, a synthetic aperture is produced by signal processing that has the effect of lengthening the antenna. Making T large makes the „synthetic aperture” large and hence a higher resolution can be achieved

Application

SAR for DEM Generation

DEM which stands for Digital Elevation Model. Two technologies can be applied to generate DEM that are stereo SAR and interferometric sar. Stereo sar uses the parallax of sar pair to generate DEM; Interferometric sar uses the different phases of two sar images to estimate the surface height. A DEM for a large area can be generated without the need of ground control or a few control points.

DEM Generation Image
 Subsidence Image
SAR for Subsidence Monitoring

Di-In-SAR technology is used The millimeters level of accuracy can be obtained This technology is good for monitoring the construction site such as mining area, city…. It can help in predicting the hazards such as mining exploitation.

SAR for Soil Moisture Content

Soil dielectric constant is calculated through the sar backscattering signals. The soil moisture content can be estimated by the soil dielectric constant. The accuracy of the estimated result depends on the SAR wavelength, the polarization used. It is useful for irrigation monitoring as well as environmental monitoring.

In the image you can see The SMAP radar image acquired from march 21 to april 3rd 2015. Weaker radar signals (shown in blue) reflect low soil moisture or lack of vegetation such as deserts.strong radar signals (shown in red) are seen in forests. SMAP’S radar also takes data over the ocean and sea.

Soil Moisture content image
Agrincultral image
SAR for Crop Estimation

Multi temporal SAR data should be used to monitor the plant growth and the plant’s biomass. The damaged area due to flooding can also be monitored. The crop producing model may be used to stimulate the plant growth and predict the crop yields.

SAR for Flood Control

SAR data is weather independent. It can be obtained before, during and after the flood event. The flood area and flood effect area can be mapped. The flood movement can be delineated

Flood Control Image