Xiaoli Ding

Dr. Xiaoli Ding

The Hong Kong Polytechnic University, Hong Kong with expertise in Geodesy and Surveying
orcid

Research Focus & Metrics

Academic Career Length

31Years (1996-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 June 2014 in Earth-Science Reviews
Verified
Journal Article
Closed access
JHJun Hu
Jun Hu
ZLZhiwei Li
Zhiwei Li
XDXiao-Li Ding
Xiao-Li Ding
JZJ.J. Zhu
J.J. Zhu
LZLei Zhang
Lei Zhang
QSQ. Sun
Q. Sun

28 July 2014 in IEEE Transactions on Geoscience and Remote Sensing
Verified
Journal Article
Closed access
MJMi JIANG
Mi JIANG
XDXiao-Li Ding
Xiao-Li Ding
Ramon HanssenRamon Hanssen
Ramon Hanssen
RMRakesh Malhotra
Rakesh Malhotra
LCLing Chang
Ling Chang
Multitemporal interferometric synthetic aperture radar (InSAR) is increasingly being used for Earth observations. Inaccurate estimation of the covariance matrix is considered to be the most important source of error in such applications. Previous studies, namely, DeSpecKS and its variants, have demonstrated their advantages in improving the estimation accuracy for distributed targets by means of statistically homogeneous pixels (SHPs). However, these methods may be unreliable for small sample sizes and sensitive to data stacks showing large time spacing due to the variability of the temporal sample. Moreover, these methods are computationally intensive. In this paper, a new algorithm named fast SHP selection (FaSHPS) is proposed to solve both problems. FaSHPS explores the confidence interval for each pixel by invoking the central limit theorem and then selects SHPs using this interval. Based on identified SHPs, two estimators with respect to the despeckling and the bias mitigation of the sample coherence are proposed to refine the elements of the InSAR covariance matrix. A series of qualitative and quantitative evaluations are presented to demonstrate the effectiveness of our method.

1 June 2018 in Remote Sensing of Environment
Verified
Journal Article
Closed access
YZYushan Zhou
Yushan Zhou
ZLZhiwei Li
Zhiwei Li
JLJia Li
Jia Li
RZRong Zhao
Rong Zhao
XDXiao-Li Ding
Xiao-Li Ding

1 February 2012 in Remote Sensing of Environment
Verified
Journal Article
Closed access
LZLei Zhang
Lei Zhang
Zhong LuZhong Lu
Zhong Lu
XDXiao-Li Ding
Xiao-Li Ding
Hyung-Sup JungHyung-Sup Jung
Hyung-Sup Jung
GFGuangcai Feng
Guangcai Feng
CLChang-Wook Lee
Chang-Wook Lee

1 January 2015 in Remote Sensing of Environment
Verified
Journal Article
Closed access
QSQ. Sun
Q. Sun
LZLei Zhang
Lei Zhang
XDXiao-Li Ding
Xiao-Li Ding
JHJ. Hu
J. Hu
ZLZhiwei Li
Zhiwei Li
JZJ.J. Zhu
J.J. Zhu

3 September 2008 in Sensors
Verified
Journal Article
Open access
PDF file
XDXiao-Li Ding
Xiao-Li Ding
ZLZhiwei Li
Zhiwei Li
JZJian-Jun Zhu
Jian-Jun Zhu
GFGuang-Cai Feng
Guang-Cai Feng
JLJiang-Ping Long
Jiang-Ping Long
Interferometric Synthetic Aperture Radar (InSAR) is a powerful technology for observing the Earth surface, especially for mapping the Earth's topography and deformations. InSAR measurements are however often significantly affected by the atmosphere as the radar signals propagate through the atmosphere whose state varies both in space and in time. Great efforts have been made in recent years to better understand the properties of the atmospheric effects and to develop methods for mitigating the effects. This paper provides a systematic review of the work carried out in this area. The basic principles of atmospheric effects on repeat-pass InSAR are first introduced. The studies on the properties of the atmospheric effects, including the magnitudes of the effects determined in the various parts of the world, the spectra of the atmospheric effects, the isotropic properties and the statistical distributions of the effects, are then discussed. The various methods developed for mitigating the atmospheric effects are then reviewed, including the methods that are based on PSInSAR processing, the methods that are based on interferogram modeling, and those that are based on external data such as GPS observations, ground meteorological data, and satellite data including those from the MODIS and MERIS. Two examples that use MODIS and MERIS data respectively to calibrate atmospheric effects on InSAR are also given.