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顺轨干涉SAR浅海地形成像建模及其最优雷达观测参数分析

于祥祯 种劲松 洪文

于祥祯, 种劲松, 洪文. 顺轨干涉SAR浅海地形成像建模及其最优雷达观测参数分析[J]. 电子与信息学报, 2010, 32(10): 2377-2382. doi: 10.3724/SP.J.1146.2009.091368
引用本文: 于祥祯, 种劲松, 洪文. 顺轨干涉SAR浅海地形成像建模及其最优雷达观测参数分析[J]. 电子与信息学报, 2010, 32(10): 2377-2382. doi: 10.3724/SP.J.1146.2009.091368
Yu Xiang-Zhen, Zhong Jin-Song, Hong Wen. Shallow Sea Topography Imaging Model by Along-track Interferometric SAR and Its Optimal Radar Parameters Analysis[J]. Journal of Electronics & Information Technology, 2010, 32(10): 2377-2382. doi: 10.3724/SP.J.1146.2009.091368
Citation: Yu Xiang-Zhen, Zhong Jin-Song, Hong Wen. Shallow Sea Topography Imaging Model by Along-track Interferometric SAR and Its Optimal Radar Parameters Analysis[J]. Journal of Electronics & Information Technology, 2010, 32(10): 2377-2382. doi: 10.3724/SP.J.1146.2009.091368

顺轨干涉SAR浅海地形成像建模及其最优雷达观测参数分析

doi: 10.3724/SP.J.1146.2009.091368
基金项目: 

微波成像技术国家重点实验室基金(9140C1901030702)资助课题

Shallow Sea Topography Imaging Model by Along-track Interferometric SAR and Its Optimal Radar Parameters Analysis

  • 摘要: 该文基于浅海海流动力模型、波流交互模型、后向散射模型以及Doppler谱模型对顺轨干涉SAR浅海地形成像进行了建模。利用建立的成像模型,在准1维近似的条件下对不同雷达频率、入射角、顺轨基线长度以及极化方式等参数对顺轨干涉SAR浅海地形成像的影响进行了探讨。在成像延时低于海面去相关时间的前提下,高频率、大入射角以及长顺轨基线条件比较适合于顺轨干涉SAR浅海地形成像;而极化方式对顺轨干涉相位变化的影响不大,如果综合考虑信噪比等因素的影响,VV极化仍是顺轨干涉SAR浅海地形成像的首选极化方式。
  • Goldstein R M and Zebker H A. Interferometric radar measurement of ocean surface currents[J].Nature.1987, 328:707-709[2]Romeiser R.[J].Hirsch O, and Gade M. Remote sensing of surface currents and bathymetric features in the German Bight by along-track SAR interferometry[C]. 2000 IEEE International Geoscience and Remote Sensing Symposium (IGARSS2000), Hawaii, Jul. 24-2.2000,:-[3]Romeiser R and Runge H. Current in European Coastal Waters and Rivers by Along-Track InSAR. In: Remote Sensing of the European Seas[M]. Springer, the Netherlands, 2008: 411-422.[4]Campbell J W M, Gray A L, and Mattar K E, et al.. Ocean surface feature detection with the CCRS along-track InSAR[J]. Canadian Journal of Remote Sensing. 1997, 23(1): 24-37.[5]范开国, 黄韦艮, 贺明霞等. SAR浅海水下地形遥感研究进展[J]. 遥感技术与应用. 2008, 23(4): 479-485.[6]Fan K G, Huang W G, and He M X, et al.. Progress on remote sensing of the shallow sea bottom topography by SAR[J]. Remote Sensing of Technology and Application, 2008, 23(4): 479-485.[7]范开国, 傅斌, 黄韦艮等. 浅海水下地形的SAR遥感仿真研究[J]. 海洋学研究, 2009, 27(2): 79-83.Fan K G, Fu B, and Huang W G, et al.. Simulation study on SAR shallow water bathymetry[J]. Journal of Marine Sciences, 2009, 27(2): 79-83.[8]傅斌. SAR浅海水下地形探测[D]. [博士论文], 中国海洋大学, 2005.[9]Fu B. Shallow sea bottom topography mapping by SAR[D]. [Ph.D. dissertation], Ocean University of China, 2005.[10]Romeiser R and Alpers W. An improved composite surface model for the radar backscattering cross section of the ocean surface 2Model response to surface roughness variations and the radar imaging of underwater bottom topography[J].. Journal of Geophysical Research.1997, 102(C11):25251-25267[11]余颖, 王小青, 朱敏慧等. 基于二阶散射的海面三尺度雷达后向散射模型[J]. 电子学报, 2008, 36(9): 1771-1775.Yu Y, Wang X Q, and Zhu M H, et al.. Three-scale radar backscattering model of the ocean surface based on second-order scattering[J]. Acta Electronica Sinica, 2008, 36(9): 1771-1775.[12]Romeiser R and Aplers W. An improved composite surface model for the radar backscattering cross section of the ocean surface 1Theory of the model and optimization/validation by scatterometer data[J].. Journal of Geophysical Research.1997, 102(C11):25237-25250[13]Romeiser R and Thompson D R. Numerical study on the along-track interferometric radar imaging mechanism of oceanic surface currents[J].IEEE Transactions on Geoscience and Remote Sensing.2000, 38(1):446-485
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出版历程
  • 收稿日期:  2009-10-22
  • 修回日期:  2010-03-16
  • 刊出日期:  2010-10-19

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