Synthetic Aperture Radar (SAR) Basics
Synthetic Aperture Radar (SAR) is an emerging technology in remote sensing.
In fact, Sentinel-1 is equipped with this active type of sensor. Likewise, Radarsat and TerraSAR use synthetic aperture radar.
The main advantage behind this technology is how it can synthetically produce higher resolution images in any weather condition and even at night.
Today, we don’t intend on getting into the precise details about how this technology works. Instead, we will interpret SAR imagery with basic examples and give some real-world applications.
SAR’s Bat-Like Capabilities
It’s said that synthetic aperture radar is similar to how bats use echolocation to navigate in a cave.
When bats fly in a cave, it uses sound to navigate. Generally, they create sound waves from 50 to 120 dB. When this sound bounces off a wall and returns to the bat, it understands distance based on the echo.
In general, the same principles apply for SAR. The satellite sends microwave pulses to Earth. The pulse return back to the satellite and the sensor makes an image from the returned echoes.
Generally, synthetic aperture radar is side-looking. This means they don’t look completely down at Nadir, but at an angle. There are advantages with this type of viewing angles which I will mention below.
Mentioned earlier, microwave radar can see at night and through clouds and smoke. At any time of the day or in any type of weather conditions, SAR works.
Actually, longer wavelengths can penetrate clouds better and even the ground. For example, L-band (~24 cm) radar has longer wavelengths than C-band (~6 cm) and X-band (~3cm).
Types of Radar Scattering
Side-looking radar interact with different types of terrain. The 3 main types of scattering mechanisms are specular, diffuse and double-bounce.
First, we will provide a schematic for each type of scattering. After, we will give an interpretation where each type of scattering occurs.
SMOOTH SURFACE reflection comes from flat terrain like roads or water. For this type of scattering, very little energy of the transmitted pulse returns back to the sensor (similar to a mirror). In this example, pixels will appear black typically with values less than -20dB.
ROUGH SURFACE scattering such as plowed farm fields and vegetation. Scattering goes in all directions diffusely. For example, typical pixel values will be greater than -20dB and in grey.
Often, DOUBLE BOUNCE occurs off structures and man-made objects. The reflected pulse hits one surface after the other and back to the sensor. For example, typical pixel values will appear white with values greater than -10dB.
SAR Image Interpretation
Now that you know a bit of the basics of synthetic aperture radar, let’s look at a SAR image with these types of scattering. In this Radarsat-2 example, the image clearly shows all three types of backscatter.
For example, this scene had a river that flows in the east-west direction. As shown in the schematic above, very little energy reflects back to the radar sensor. In this case, the pixel is dark with a low dB.
This can also be seen in the south-east portion with the road/airport paved surface. Again, this is specular reflection off of a smooth surface.
On the other hand, the bright white in the center of image can be interpreted as an urban feature. The radar is receiving double-bounce backscatter, meaning the transmitted pulses are returning back to the sensor.
It’s unclear at this scale what this object is but it’s due to double-bounce returns. Because of its values greater than -10dB, pixels will appear as a bright white.
Finally, the majority of the radar image is rough surface scattering. You have a bit of specular and double-bounce scattering.
This may be from annual cropland, vegetation or grasses or other features. It is diffuse scattering because there’s not a high or low amount of backscatter in the image.
Synthetic Aperture Radar Example Applications
How can we apply these SAR concepts to real world applications?
There are hundreds of remote sensing applications. Likewise, SAR has applications in environment, safety, military and more. Actually, the first one shares the same acronym as SAR (search and rescue).
In search and rescue missions, weather conditions are often poor. In the case of forest fires, smoke could completely block visibility. Because microwave SAR is not affected by these types of conditions, rescuers use it to find man-made objects on the ground. Specifically, it looks for double-bounce scattering where the crash site occurred. Or even where flooding occurs, if there is specular reflection (dark pixels).
Scientists use synthetic aperture radar to estimate surface elevation with the Space Shuttle Radar Topography Mission inSAR. This satellite used interferometry (inSAR) generating one of the most accurate elevation models of the whole globe. In addition, scientists use inSAR for terrain displacement based on phase differences.
As shown above, SAR is about understanding surface characteristics based on backscatter. That’s why we use SAR during oil spills and to understand ocean waves. During an oil spill, oil floats on water suppressing waves. Using synthetic aperture radar, this creates a smoother surface, appearing dark in the radar image. But if you were searching for a ship in the Arctic, you’d look for double-bounce or bright pixels in a SAR image.
Lastly, microwave radar is sensitive to the dielectric constant in features. This is why researchers are trying to study soil moisture using synthetic aperture radar. In agriculture, farmers can use this to understand wetness in the first few centimeters of a bare soil profile. Even for mapping wetlands, scientists use Touzi decomposition technique.
A Little Deeper in the Technology
Polarization refers to the orientation of the radar wave from the SAR antenna. Both electric and magnetic lines of force are at right angles to each other, but it’s the electric field determines the direction of polarization of the wave. Synthetic Aperture Radar uses an antenna that can transmit in either the horizontal (H) or vertical (V) polarization.
When the electromagnetic wave scatters from a target, the polarisation state of an electromagnetic wave can change. When the sensor receives the returning wave, it measures the degree in change in polarisation from the target. For example, it can either be H or V polarization or both simultaneously.
For single polarization, these are typical transmit and receive pairs.
- HH – for horizontal transmit and horizontal receive
- VV – for vertical transmit and vertical receive
- HV – for horizontal transmit and vertical receive
- VH – for vertical transmit and horizontal receive
The advantage is that you can infer more information of the surface characteristics. For example, we can do use decomposition techniques like Freeman-Durden to obtain how much surface, double-bounce and volume scattering in a SAR image.
Finally, it’s “synthetic aperture” because it can create higher resolution images. Because it receives backscatter along the length of the synthetic aperture radar, it can synthetically generate a higher resolution image for a point target on Earth. The entire length of the synthetic aperture radar has the backscatter information for the point target. When all the backscatter information is merged, it’s like a “synthetic aperture”.
Without experience in radar, it may look like a bunch of pixels. You don’t get a pretty picture used in a map.
Regardless, radar images can be noisy and often require smoothing. But using decomposition techniques and a bit of SAR interpretation, suddenly SAR images become a valuable tool.
If you want to try to use synthetic aperture radar, take a look at our list of 15 free satellite imagery sources.