2022
DOI: 10.3390/rs14132987
|View full text |Cite
|
Sign up to set email alerts
|

Monitoring Regional-Scale Surface Deformation of the Continuous Permafrost in the Qinghai–Tibet Plateau with Time-Series InSAR Analysis

Abstract: As an important indicator of permafrost degradation, surface deformation is often used to monitor the thawing and freezing process in the permafrost active layer. However, due to the large area of the continuous permafrost of the Qinghai–Tibet Plateau (QTP) and the large amount of data processed by conventional time-series InSAR, previous studies have mostly focused on local area investigations, and regional characteristics of surface deformation of the continuous permafrost area on the QTP are still unclear. … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
4
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 7 publications
(4 citation statements)
references
References 42 publications
0
4
0
Order By: Relevance
“…The DInSAR idea is to form an interferometric pair of two radar images before and after deformation in the same area with different time phases, and to obtain the deformation information by removing the interferometric phases generated by the terrain using a known external DEM of the same area. The main steps include: Image pair alignment, interferogram generation, simulated decoupling of terrain phases, extraction of deformation phases, geocoding, etc (Xu et al, 2022). Figure 4 shows the processing flow of DInSAR technology to extract the surface deformation area of the mine.…”
Section: Dinsar Data Processingmentioning
confidence: 99%
“…The DInSAR idea is to form an interferometric pair of two radar images before and after deformation in the same area with different time phases, and to obtain the deformation information by removing the interferometric phases generated by the terrain using a known external DEM of the same area. The main steps include: Image pair alignment, interferogram generation, simulated decoupling of terrain phases, extraction of deformation phases, geocoding, etc (Xu et al, 2022). Figure 4 shows the processing flow of DInSAR technology to extract the surface deformation area of the mine.…”
Section: Dinsar Data Processingmentioning
confidence: 99%
“…LiCSAR, an acronym for looking into continents from space with synthetic aperture radar, is a sophisticated operating system specially designed for the large-scale interferometric processing of Sentinel-1 data [41]. It is designed to automatically generate unwrapped and geocoded interferograms, as well as coherence coefficient maps, with a spatial resolution of 0.001 • (about 110 m at the equator) in the WGS-84 coordinate system [47,52]. The LiCSAR processing chain uses a variety of custom tools and algorithms source codes for the core processing functions, which are based on the advanced commercial SAR processing software, GAMMA (https://www.gamma-rs.ch/software, accessed on 26 July 2023), and consist of four main processes, i.e., Preparation of Frame Epoch SLC, Resampling to RSLC, Formation of Differential Interferograms, and Unwrapping Interferograms [42].…”
Section: Surface Uplift or Settlement Calculationmentioning
confidence: 99%
“…In addition, LiCSBAS supports the use of the Generic Atmospheric Correction Online Service (GACOS) for InSAR for atmospheric phase removal [45,46]. Considerable results have been achieved based on the research and application of LiCSAR products and LiCSBAS tools [47][48][49][50][51], including work in permafrost regions [52]. By leveraging these technological advancements, the pressure of traditional desktop-side data processing can be reduced, and the efficiency and accuracy of InSAR processing can be improved, paving the way for future research and practical applications.…”
Section: Introductionmentioning
confidence: 99%
“…Synthetic aperture radar (SAR) interferometry (InSAR) is an efficient approach for investigating large-scale displacement of the permafrost. Multi-temporal InSAR (MT-InSAR) techniques, such as persistent scatterer interferometry (PSI) [ 13 ], and the Small BAseline Subset (SBAS) method [ 14 ], have been developed to monitor spatio-temporal seasonal freeze-thaw deformations and estimate the active layer thickness (ALT) of the permafrost on the QTP [ 15 , 16 , 17 , 18 , 19 , 20 , 21 , 22 , 23 , 24 , 25 ]. In these studies, deformation monitoring of the Qinghai-Tibet Railway, the Qinghai-Tibet Highway, and their surrounding permafrost regions was carried out using multi-source SAR data and various MT-InSAR methods with different spatio-temporal scales.…”
Section: Introductionmentioning
confidence: 99%