差分干涉雷达遥感在地质学中的应用研究
|
摘要
雷达差分干涉测量是当前雷达遥感的热点研究领域 ,对地质学特别是地震、火山、大地构造的研究具有极其重要的意义。文章对差分干涉雷达遥感的原理及具体实现进行了深入研究 ,并分析了差分干涉测量结果的误差 ,着重阐述了差分干涉雷达遥感在地震、地表形变测量、火山监测、板块构造研究中的应用。
Radar differential interferometry is an up to date frontier research for radar remote sensing. It is grandly significant to earth sciences, especially to seismology, volcano, tectonics and crust deformation studies. In this paper, the mechanism and operational procedure of radar differential interferometry are introduced. The errors of measurement result of radar differential interferometry are analyzed. The emphasis is paid to the applications to seismology, volcano, tectonics and crust deformation studies. Finally, the characteristics and limitation are analyzed.
Radar differential interferometry is an up to date frontier research for radar remote sensing. It is grandly significant to earth sciences, especially to seismology, volcano, tectonics and crust deformation studies. In this paper, the mechanism and operational procedure of radar differential interferometry are introduced. The errors of measurement result of radar differential interferometry are analyzed. The emphasis is paid to the applications to seismology, volcano, tectonics and crust deformation studies. Finally, the characteristics and limitation are analyzed.
引文
[1] GabrielA K,GoldsteinR M,ZebkerH A.Mapping small ele-vation changes over large areas:Differential radar interferome-try[J].J.Geophys.Res.,1989,94(B7):9183-9191.
[2]WangChao.DEM Generation usingSIR-C/X-SAR interfer-ometric data[J].Journal ofRemoteSensing,1997,1(1):46-49.
[3]GensR,GenderenV J.SAR interferom etry-issues,tech-niques,applications[J].IntJRem oteSensing,1996,17(10):1803-1835.
[4] Kim uraH,TodoM.BaselineEstimationUsingGroundPointsforInterferom etricSAR[A].IGRASS'97,1997:442-444.
[5] GoldsteinR M,ZebkerH A,WernerC L.Satellite radar in-terferometry:two-dimensional phase unwrapping[J].RadiSci.,1988,23(4):713-720.
[6]ZebkerH A,VillasenorJ.Decorrelation in interferometricradar echoes.IEEE Trans[J].Geosci.RemoteSensing,1992,30(5):950-959.
[7] ZebkerH A,GoldsteinR M.Topographic mapping from inter-ferom etric synthetic sperture radar observations[J].J.Geo-phys.Res.,1986,91(B5):4993-4999.
[8] ZebkerH A,RosenP,GoldsteinR M,etal.On the derivationof coseismic displacement fields using differential radar inter-ferom etry:TheLanders earthquake[J].J.Geophys.Res.,1994,99:19617-19634.
[9] ZhangJin-fa,ShaoYun.SAR Interferometry andItsApplica-tionReview[J].Seismology andGeology,1998,20(3):277-288.
[10] MassonnetD,RossiM,CarmonaC,etal.The displacementfield of theLanders earthquake mapped by radar interferom etry[J].Nature,1993,34(6433):138-142.
[11] RossS L,ChristopherD E.RemoteSensingChangeDetec-tion:EnvironmentalMonitoringMethods andApplications[M].London:Taylor&F rancisLtd.,1GunpowderSquare,EC4A 3DF ,1999.
[12] MassonnetM,BrioleP,ArnaudA.Deflation ofMountEtnaMonitored bySpaceborneRadarInterferometry[J].Nature,1995,375:567-570.
[13] WernerL,RosenP,HensleyS,etal.Detection of aseismiccreep along theSanAndreas fault nearParkefield,CaliforniawithERS-1radar interferometry[A].3rdERS Symposium'Space at theSERice of ourEnvironment.'1997.
[14] MeyerB,ArmijoR,MassonnetD,etal.The1995Grevena(NorthernGreece) earthquake:F ault m odel constrained withtectonic observations andSAR interferometry[J].GeophysicalResearchL etters,1996,23(19):2677-2680
[2]WangChao.DEM Generation usingSIR-C/X-SAR interfer-ometric data[J].Journal ofRemoteSensing,1997,1(1):46-49.
[3]GensR,GenderenV J.SAR interferom etry-issues,tech-niques,applications[J].IntJRem oteSensing,1996,17(10):1803-1835.
[4] Kim uraH,TodoM.BaselineEstimationUsingGroundPointsforInterferom etricSAR[A].IGRASS'97,1997:442-444.
[5] GoldsteinR M,ZebkerH A,WernerC L.Satellite radar in-terferometry:two-dimensional phase unwrapping[J].RadiSci.,1988,23(4):713-720.
[6]ZebkerH A,VillasenorJ.Decorrelation in interferometricradar echoes.IEEE Trans[J].Geosci.RemoteSensing,1992,30(5):950-959.
[7] ZebkerH A,GoldsteinR M.Topographic mapping from inter-ferom etric synthetic sperture radar observations[J].J.Geo-phys.Res.,1986,91(B5):4993-4999.
[8] ZebkerH A,RosenP,GoldsteinR M,etal.On the derivationof coseismic displacement fields using differential radar inter-ferom etry:TheLanders earthquake[J].J.Geophys.Res.,1994,99:19617-19634.
[9] ZhangJin-fa,ShaoYun.SAR Interferometry andItsApplica-tionReview[J].Seismology andGeology,1998,20(3):277-288.
[10] MassonnetD,RossiM,CarmonaC,etal.The displacementfield of theLanders earthquake mapped by radar interferom etry[J].Nature,1993,34(6433):138-142.
[11] RossS L,ChristopherD E.RemoteSensingChangeDetec-tion:EnvironmentalMonitoringMethods andApplications[M].London:Taylor&F rancisLtd.,1GunpowderSquare,EC4A 3DF ,1999.
[12] MassonnetM,BrioleP,ArnaudA.Deflation ofMountEtnaMonitored bySpaceborneRadarInterferometry[J].Nature,1995,375:567-570.
[13] WernerL,RosenP,HensleyS,etal.Detection of aseismiccreep along theSanAndreas fault nearParkefield,CaliforniawithERS-1radar interferometry[A].3rdERS Symposium'Space at theSERice of ourEnvironment.'1997.
[14] MeyerB,ArmijoR,MassonnetD,etal.The1995Grevena(NorthernGreece) earthquake:F ault m odel constrained withtectonic observations andSAR interferometry[J].GeophysicalResearchL etters,1996,23(19):2677-2680
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心