SAR-Synthetic Aperture Radar
I just came back from a summer school in Germany and wanted to share with you the topic that accompanied me during this week. Radar remote sensing still belongs to one of the less discussed issues in the geospatial domain. The reasons therefore are diverse. The radar based technique implies not only a highly specialised form of remote sensing application but also sound knowledge about the physics and processing behind. Thus, it is often associated with discomfort in the geospatial community, while for a broad majority it is still an unknown issue. Indeed, radar remote sensing is something very ‘technical’ meaning that it does not need a natural source of radiation and runs completely man made working with an active and passive mode of sending and receiving exactly one wave length (in the microwave spectrum). The technology completely relies on the physics of electromagnetic waves, which is a huge advantage of radar: We are talking about exact measurements when the backscattered wave is compared to the sent one concerning its physics and the time response and thus have exact results.
Meaningful for the reflection of radar waves on the surface are the presence of (liquid) water (di-electric objects), the size of an object and the roughness of the surface. The system itself always emits the radar wave on one side. These characteristics explain the backscattering behaviour of the waves that finally makes up a radar image. To describe some scenarios, flat water reflects the radar waves into outer space according to the arrival angle (mirror effect), whereas the front side of ocean waves will return the radar waves back to the sensor. Ice (crystalline water) is penetrated as any other solid object lacking water, which explains the use of radar satellites for assessing the ice masses of the poles. The penetration properties of vegetation depend on the kind of green structures and the wavelength. The rule here is that only objects of at least the same size as the radar wave length may facilitate reflection. Accordingly, small vegetation structures such as crops or meadows reflect small wavelengths (X-band) and are permeable for long ones (L-band), while forests reflect small wave lengths, though not always on the canopy surface, and long wave lengths are only backscattered by stems and big trunk structures.
Applications in science and engineering
The characteristics of radar make the technology useable for a vast range of applications in the civilian sector (see points below). Due to its sensitivity to water and artificial objects as well as the independency from sun radiation (possibility to also scan by night) radar is also used for military purposes.
- Sea ice monitoring
- Glacier monitoring
- Snow features
- Water bodies, floodings
- Ocean wave spectra
- Soil Moisture
- Topography – the SRTM is based on radar information
- Surface deformation detection (interferometry- InSAR)
- Crop production forecasting
- Forest cover mapping
- Coastal surveillance (erosion)
- Monitoring disasters such as forest fires, floods, volcanic eruptions, and oil spills
- Urban planning
Some examples to demonstrate the specificities of radar remote sensing.
After four days of education I was impressed by the range of possibilities in radar remote sensing. During the week I found out that radar technique indeed is a complex application, though learnable and for the usage you dont’t have to be an electrical engineer/physicist as it is sufficient to get into the mathematical and physical basics step by step. Radar is still a young technique and a lot of research is done to improve application and sensor technique. Hence, it is going to offer a lot of opportunities of research and finally employment in the future.
The SAR Summer School was organised by University of Jena and German Aerospace Centre (DLR). This year it was held the first time. For those interested to attend the course next year, click here.
SOME TECHNICAL ADDITIONS
SAR – Synthetic Aperture Radar refers to the fact that one point is captured several times separately. This enhances the spatial resolution in azimuth direction (flying direction of the satellite) compared to a real aperture radar.
Most used wavelengths
Finally some polar orbiting missions:
First sensor SeaSAT (1976)
Actual radar missions
Italy COSMO Sky-Med (2007)
India RISAT-1 (2012)
ESA Sentinel 1 (2014)
Japan Alos 2 (2013)