IEEE Geoscience and Remote Sensing Magazine - March 2020 - 31
a 3 × 3 patch. After formulating the joint pixel patch, SHP
identification and phase optimization are performed by the
time-series likelihood ratio test and the joint-subspace projection method, respectively. Using the coherence information from neighboring pixel stacks, JSInSAR is able to provide
reliable parameters estimation even in the presence of some
coregistration errors.
PERSISTENT SCATTERER PAIR
The most important feature of the PSP method is that it defines and uses PS pairs to identify PSs. It overcomes the misselection and omission caused by PS identification based
on amplitude and improves the accuracy of the parameter
solution [74], [75]. The core step of the PSP algorithm is to
establish the PSP network using an iteration method. In the
iteration, the deformation rate and elevation correction are
estimated by maximizing the phase coherence. When the
coherence coefficient is greater than the given threshold,
ux(5)
the PS pair is added to a set. This process is repeated until
no new point pairs can be added. At the same time that the
iteration is completed, the parameters of the entire scene
are obtained. Table 1 compares of various time-series InSAR techniques.
OTHER MATTERS
In addition to the complete time-series InSAR frameworks mentioned previously, there are also some minor
improvements to the time-series InSAR technique. In
[76], the periodic deformation caused by seasonal temperature variation can be solved on the basis of the PSI
technique. Some methods consider high-order deformation models, such as deformation acceleration [77].
In [78]-[80], a temperature model incorporated into the
phase model to estimate the thermal expansion component of the building is considered. To avoid local extremums, the authors in [81] applied a particle swarm
SLC 1
SLC k
SLC N
1-1 2-1 3-1
1-k 2-k 3-k
1-N 2-N 3-N
4-1 5-1 6-1
4-k 5-k 6-k
4-N 5-N 6-N
7-1 8-1 9-1
7-k 8-k 9-k
7-N 8-N 9-N
1-1
1-k
1-N
5-1
5-k
5-N
9-1
9-k
9-N
FIGURE 13. The formulation of a joint pixel vector using a 3 × 3 patch. SLC: single look complex.
TABLE 1. A COMPARISON OF TIME-SERIES INSAR TECHNIQUES.
METHOD
INTERFEROGRAM
MODE
MEASUREMENT
POINT
DEFORMATION MODEL
PHASE UNWRAPPING
OPTIMIZER
PSI
Single reference
PS
Linear model in time
1D time
Periodogram
SBAS
Multireference
DS
Linear model in time
2D space
MCF + SVD
CPT
Multireference
PS and DS
Linear model in time
1D time
Conjugate gradient
PSP
Single reference
PS
Linear model in time
1D time
Periodogram
SqueeSAR
Single reference
DS
Linear model in time
1D time
Periodogram
JSInSAR
Single reference
DS
Linear model in time
1D time
Periodogram
StaMPS
Single reference
PS
Spatial smoothness
2D space + 1D time
Filtering
QPS
Multireference
PS and DS
Linear model in time
1D time
Least square
TCP-InSAR
Multireference
PS
Linear model in time
None
Least square
MTDA
Multireference
PS
Spatial smoothness
2D space + 1D time
MCF
STUN
Single reference
PS
Linear model in time
2D space + 1D time
LAMBDA
LAMBDA: least squares ambiguity decorrelation adjustment.
MARCH 2020
IEEE GEOSCIENCE AND REMOTE SENSING MAGAZINE
31
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