期刊文献+

C-band和L-band雷达干涉数据西部冰川区域相干性对比分析 被引量:10

A COMPARATIVE STUDY OF COHERENCE PATTERNS OF C-BAND AND L-BAND INTERFEROMETRIC SAR IN WESTERN GLACIER AREAS
下载PDF
导出
摘要 干涉雷达相干性问题是制约利用干涉方法提取中国内陆冰川相关参数的重要原因。本文在理论分析干涉空间失相干因素的基础上,从垂直基线、地面坡度和波长3个方面对比了雷达干涉数据在内陆冰川表面的干涉特性。以中国西部典型的内陆冰川(冬克玛底冰川)为研究区域,采用C-band的ENVISAT/ASAR和L-band的ALOS/PALSAR数据,对比分析二者在冰川区域相干性的差别,并给出了量化结果。研究表明,相比于C-band雷达干涉数据,L-band雷达干涉数据在内陆冰川区域具有更强的抗失相干的能力,更适合于内陆冰川相关参数的提取。 Decorrelation is one of the key restrictive factors when the InSAR technique is used to derive the parameters of inland glaciers in China.This paper has compared the coherence patterns between different perpendicular baselines,terrain slopes and wavelengths from both the theoretical and the experimental results based on analyzing the factors leading to the interferometric spatial decorrelation.Taking the Dongkemadi Glacier of western China as the study area,the authors analyzed the different coherence patterns of the Dongkemadi Glacier by using C-band ENVISAT/ASAR and L-band ALOS/PALSAR data.The quantitative result is also given.The results indicate that the capability of the coherence by ALOS/PALSAR repeat-pass pairs is higher than that of the coherence by ENVISAT/ASAR pairs.The L-band ALOS/PALSAR data are more fit for extracting the parameters of the inland glacier.
出处 《国土资源遥感》 CSCD 2009年第2期9-13,18,共6页 Remote Sensing for Land & Resources
基金 国家重点基础研究发展计划(2009CB723901) 国家自然科学基金(40671140) 中国科学院知识创新工程重要方向项目(KZCX2-YW-301) 中国科学院遥感应用研究所知识创新项目(08S03100CX)共同资助
关键词 雷达干涉测量 失相干 相干特性分析 SAR interferometry Decorrelation Analysis of the coherence patterns
  • 相关文献

参考文献16

  • 1[1]Zebker H A,Goldstein R M.Topographic Mapping from Interferometric Synthetic Aperture Radar Observations[J].Journal of Geophysical Research,1986,91(B5):4993-4999.
  • 2[2]Eldhuset K,Andersen P,Hauge S,et al.ERS Tandem InSAR Processing for DEM Generation,Glacier Motion Estimation and Coherence Analysis on Svalbard[J].International Journal of Remote Sensing,2003,24(4):1415-1437.
  • 3[3]Goldstein R,Engelhard R,Kamb B,et al.Satellite Radar Interferometry for Monitoring Ice Sheet Motion:Application to an Antarctic Ice Stream[J].Science,1993,262(10):1525-1530.
  • 4[4]Joughin I,Tulaczyk S,Fahnestock R,et al.A Mini-surge on the Ryder Glacier,Greenland,Observed by Satellite Radar Interferometry[J].Science,1996,274(10):228-230.
  • 5[5]Joughin I,Winebrenner D,Fahnestock M,et al.Measurement of Ice-sheet Topography Using Satellite-radar Interferometry[J].Journal of Glaciology,1996,42(140):10-22.
  • 6[6]Joughin I,Kwok R,Fahnestock M.Estimation of Ice-sheet Motion Using Satellite Radar Interferometry:Method and Error Analysis with Application to Humboldt Glacier,Greenland[J].Journal of Glaciology,1996,42(142):564-575.
  • 7[7]Joughin I R,Winebrenner D P,Fahnestock M A.Observations of Ice-sheet Motion in Greenland Using Satellite Radar Interferometry[J].Geophysical Research Letters,1995,22(5):571-574.
  • 8[8]Kwok R,Fahnestock M A.Ice Sheet Motion and Topography from Radar Interferometry[J].IEEE Transactions on Geoscience and Remote Sensing,1996,34(1):189-200.
  • 9[9]Kwok R,Siegert M J,Carsey F D.Ice Motion Over Lake Vostok,Antarctica:Constraints on Inferences Regarding the Accreted Ice[J].Journal of Glaciology,2000,46(155):689-694.
  • 10[10]Rignot E,Gogineni S,Krabill W,et al.North and Northeast Greenland Ice Discharge from Satellite Radar Interferometry[J].Science,1997,276(5):934-937.

二级参考文献4

  • 1姚檀栋,青藏高原冰川气候与环境,1993年,22页
  • 2丁良福,青藏原冰川气候与环境,1993年,96页
  • 3杨针娘,中国冰川水资源,1991年,83页
  • 4杨大庆,冰川冻土,1988年,10卷,4期,384页

共引文献43

同被引文献134

引证文献10

二级引证文献88

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部