Deformation analysis of the seawall in Qiantang estuary with multi- temporal InSAR
Deformation analysis of the seawall in Qiantang estuary with multi- temporal InSAR
- 2015年19卷第2期 页码:339-346
纸质出版:2015
移动端阅览
纸质出版:2015
移动端阅览
Deformation monitoring is essential to the safe operation of seawalls. This paper reports the Interferometric Synthetic Aperture Radar( InSAR) measurement results derived from 31 Envisat ASAR images acquired over Hang zhou from 2006 to 2010
with special focus on the seawall in the Qiantang Estuary. Multi-temporal InSAR( MTInSAR) was used to extract deformation information from both Persistent Scatterers( PSs) and Distributed Scatterers( DSs)
which provide dense measurement of the deformation of the seawall. Compared with the leveling measurement at 28 points
the mean error derived by InSAR is 0. 436 mm
with the largest error of 5. 016 mm
which confirms the millimeter-level precision and accuracy of the InSAR technique. A time series analysis was conducted based on these two datasets
and results showed that the subsidence of seawalls was spatially continuous and had a local negative unimodal pattern with distance. A linear tendency with minor local fluctuation was also observed in the time domain during a period of nearly seven years.
Deformation monitoring is essential to the safe operation of seawalls. This paper reports the Interferometric Synthetic Aperture Radar( InSAR) measurement results derived from 31 Envisat ASAR images acquired over Hang zhou from 2006 to 2010
with special focus on the seawall in the Qiantang Estuary. Multi-temporal InSAR( MTInSAR) was used to extract deformation information from both Persistent Scatterers( PSs) and Distributed Scatterers( DSs)
which provide dense measurement of the deformation of the seawall. Compared with the leveling measurement at 28 points
the mean error derived by InSAR is 0. 436 mm
with the largest error of 5. 016 mm
which confirms the millimeter-level precision and accuracy of the InSAR technique. A time series analysis was conducted based on these two datasets
and results showed that the subsidence of seawalls was spatially continuous and had a local negative unimodal pattern with distance. A linear tendency with minor local fluctuation was also observed in the time domain during a period of nearly seven years.
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