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???????編???InSAR???????У???????о?
引用本文:李永生,张景发,姜文亮,罗毅,王晓醉.???????編???InSAR???????У???????о?[J].大地测量与地球动力学,2015,35(1):145-149.
作者姓名:李永生  张景发  姜文亮  罗毅  王晓醉
作者单位:1 中国地震局地壳应力研究所(地壳动力学重点实验室), 北京市安宁庄路1号, 100085 
2 中国地震局工程力学研究所, 哈尔滨市学府路29号, 150080
3 武汉大学科学技术发展研究院, 武汉市珞喻路129号, 430079
基金项目:国家自然科学基金(41204004);中央公益性科研院所基本科研业务费专项(ZDJ2013-22);国家科技部、欧洲空间局龙计划三期(10607)
摘    要:????????λ???????????????3????????????????????編???н??????????????????????????????????2007~2010?????20??ENVISAT ASAR?????÷????????????????????Э??????????У?????????????????й????????????Э?????????????????????3.1 mm2??????0.6mm2????????80%??e-folding???????????1.5 km?????0.21 km????????86%????????編??????Ч??У????????е??????λ?????

关 键 词:?????????  ?????????????  ?????????????  ??????λ???  
收稿时间:2014-02-12

Atmospheric Artifacts Correction in Time Series InSAR Using Network Methodology
LI Yongsheng,ZHANG Jingfa,JIANG Wenliang,LUO Yi,WANG Xiaozui.Atmospheric Artifacts Correction in Time Series InSAR Using Network Methodology[J].Journal of Geodesy and Geodynamics,2015,35(1):145-149.
Authors:LI Yongsheng  ZHANG Jingfa  JIANG Wenliang  LUO Yi  WANG Xiaozui
Institution:1 Key Laboratory of Crustal Dynamics, Institute of Crustal Dynamics, CEA,1 Anningzhuang Road, Beijing 100085,China
2 Institute of Engineering Mechanics, CEA, 29 Xuefu Road,Harbin 150080,China
3 College of Science and Technology Development,Wuhan University,129 Luoyu Road,Wuhan 430079,China
Abstract:As a consequence of variability in water vapor content in the atmosphere, phase artifacts in interferometric synthetic aperture radar (InSAR) images (which are caused by path delays as the radar signal propagates through the stratified and turbulent atmosphere and ionosphere), frequently degrade the interpretability of the phase and correlation signatures of terrain. The effect of atmospheric delay consists of three parts. In this paper, the three phase delays are calculated using network methodology respectively. It is applied to 20 scenes of ENVISAT (ASAR) images from 2007 to 2010 over the Bengco zone of Tibet. The 1-D covariance function is used to estimate atmosphere artifacts. The experimental results suggest that after atmospheric effects are mitigated, the mean variance of the exponential function of the interferograms is reduced from 3.1mm2 to 0.6mm2, and the average e-folding wavelength is reduced from 1.5 km to 0.21 km, which means the APS correction has reduced the mean amplitude and wavelength of the covariance by about 80% and 86%, respectively.
Keywords:network methodology  long wavelength phase delay  topography correcting atmospheric delay  atmospheric turbulence artifacts
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