Extracting the most from satellite radar data.
SqueeSAR™ is the latest algorithm developed by TRE for processing satellite radar data to produce quantitative ground deformation maps. Learn more about the SqueeSAR™ algorithm.
SqueeSAR™ results can be visualized as maps of ground deformation (for an overview of ground motion over the entire area processed) or as time-series of individual ground point displacements.
Deformation maps can be easily imported and visualized in ArcGIS. Learn more about map visualization.
The two principle results of SqueeSAR™ analysis are:
- Average velocity map
- Time Series (for each measurement point)
For each data delivery, the position of each measurement point (latitude, longitude, elevation) and standard deviation map are provided with the SqueeSAR™ database.
In addition to the principle results, the following SqueeSAR™ maps can also be provided according to the ground movement expected and interest in particular features:
- Cumulative displacement
- Average acceleration
- Periodic variation (seasonality) amplitude
- Differential displacement
Below is a description of the individual maps:
The average velocity field is used to map the average displacement rate of each ground point identified in SqueeSAR™ analysis over the time period of satellite imagery analyzed. By analyzing the cumulative displacement and average velocity fields it is possible to identify and map areas of subsidence, uplift and stability.
The color scale applied to the image is calculated according to the maximum and minimum data values. In analyzing all SqueeSAR™ data fields, ground displacement behavior can be detected and characterized.
Example: average velocity map
A time series is provided for each ground measurement point identified with SqueeSAR™ analysis. Time series describe the evolution of displacement over the entire analyzed period - information that cannot be extracted solely from analysis of the average velocity, cumulative displacement or average acceleration field.
Each point on a time series corresponds to a single satellite acquisition. Analyzing a time series, it is possible to identify non-linear movement, seasonal trends, ground acceleration and detect sharp changes in movement.
Example: time series
Maps of elevation are provided for each ground measurement point obtained from SqueeSAR™ analysis. The color scale is calculated according to the maximum and minimum data values and represents elevation with respect to the ellipsoid model WSG84.
Elevation values are particularly useful in Single Building and infrastructure stability analysis in understanding the position of measurement points on a structure.
Examples: elevation and elevation - single building
Each measurement calculated from SqueeSAR™ data has an associated standard deviation value. The standard deviation is a measurement of the dispersion of an estimated value and provides an idea of how reliable each individual point is – the lower the value, the more reliable the information provided.
The color scale applied to the image is calculated according to the maximum and minimum data values. As a general rule of thumb, as with most common geodetic networks, the standard deviation increases the further its position from the chosen reference point.
Example: standard deviation
The cumulative displacement field is used to map the total displacement that has occurred from the first satellite image acquired, to any sequential acquisition (from the second to the last). Cumulative displacement maps allow the evolution of subsidence, uplift and stability to be characterized over time.
The color scale applied to the image is calculated according to the maximum and minimum data values. In analyzing all SqueeSAR™ data fields, ground displacement behavior can be detected and characterized.
Example: cumulative displacement map
The acceleration field maps the average change in velocity over the time period of satellite imagery analyzed, for each ground measurement point identified. The acceleration field highlights areas affected by increasing or decreasing rates of velocity.
The color scale applied to the image is calculated according to the maximum and minimum data values. In analyzing all SqueeSAR™ data fields, ground displacement behavior can be detected and characterized.
Example: average acceleration map
The periodic variation amplitude (or seasonality amplitude) highlights areas within the data that exhibit cyclic behavior. The seasonality field allows the identification of periodic displacements and seasonal deformation that may not be visible in other data fields.
The color scale applied to the image is calculated according to the maximum and minimum data values. In analyzing all SqueeSAR™ data fields, ground displacement behavior can be detected and characterized.
Example: periodic variation (seasonality) amplitude
Maps of differential displacement allow displacements that have occurred between two single satellite acquisitions (two discreet time periods) to be mapped and analyzed. This process can be performed for each image pair in a data set and is useful for the identification of spatial distribution of discreet displacement events.
Color scale is calculated according to the maximum and minimum data values.
Example: differential displacement