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1.
The impact of wave spectra modulation transfer function (MTF) in shoreline change model accuracy has been presented. The MTF consisted of real aperture radar (RAR) and velocity-bunching which is utilized to map the wave spectra observed from ERS-1 into the observed real ocean wave spectra. Based on this information, the shoreline change model have developed. Two hypotheses were concerned with the shoreline change model based on ERS-1 wave spectra. First, there is a significant difference between RAR and velocity-bunching modulations for ERS-1 wave spectra modeling. Second, this significant difference is induced a different spatial variation for shoreline change pattern.This study shows that there was the significant difference between velocity-bunching and quasi-linear models. The study shows that velocity-bunching model produces wave spectra pattern approximately close to the real ocean wave compared to the quasi-linear model. The error percentage occurred with velocity-bunching and quasi-linear models were 33.5 and 46.7%, respectively. The highest rate of erosion occurred to the shore south of Chendering with −5 m per year and the highest rate of sedimentation occurred to north of Chendering headland with 3 m per year. It can be concluded that ERS-1 data could be used to model shoreline change and identify the locations of erosion and sedimentation. The sedimentation was occurred due to the effect of lowest wave spectra energy captured along the range direction while the erosion was occurred due to highest spectra energy captured near azimuth direction.  相似文献   

2.
SAR海洋内波表层流反演方法探讨   总被引:3,自引:0,他引:3  
范开国 《遥感学报》2010,14(1):127-139
基于海洋内波SAR成像机理与M4S海面微波散射成像模型,提出SAR海洋内波表层流反演新方法。首先从SAR图像上获得内波剖面的海面后向散射强度,利用AH理论的线性近似关系得到猜测表层流,通过海面微波散射成像模型仿真海洋内波的SAR海面后向散射强度,利用二分法不断地修改风速和流速梯度等参数,使仿真信号最大程度的逼近实际SAR图像上的海面后向散射强度,输出最终海表层流。以中国南海海区3景海洋内波SAR图像为例,对该方法进行了探讨。结果表明,仿真的海洋内波SAR海面后向散射强度剖面和实际SAR图像上的信号剖面吻合,两者的相关系数达90%以上,说明该反演方法是收敛与可行的。  相似文献   

3.
The present work was aimed to compare the abilities of radar and optical satellite data to estimate crop canopy cover, which is a key component of productivity estimates. Three ERS-1 SAR images were obtained of East Anglia (UK) in 1995 and one ERS-2 SAR image in 1996. The images covered a study area around the IACR Brooms Barn Sugar Beet Research Institute. Field data comprising radiometric and biophysical measurements of the crop canopy were collected in two fields from June 22 to August 3, 1995 to coincide with ERS-1 SAR overpass dates. In 1996, field data were collected in two fields from June 11 to July 29 on a weekly basis. A previously calibrated version of the water cloud model was inverted to estimate Leaf Area Index (LAI) from ERS-1 and ERS-2 SAR backscatter and soil moisture samples. Canopy cover was estimated from the radar-estimated LAI using a standard exponential relationship that has a well-established coefficient for sugar beet. Radio-metrically and atmospherically corrected data from three SPOT images in 1995 and one SPOT image in 1996 were used to calculate the Optimised Soil Adjusted Vegetation Index (OSAVI), from which crop canopy cover was estimated using a relationship determined previously by canopy modelling. The crop cover values estimated by satellite were in good agreement with those measured on ground with the Parkinson radiometer. Radar data may be able to provide useful estimates of canopy cover for crop production modelling, especially in the case of loss of optical data due to cloud.  相似文献   

4.
Gaussian smoothed SAR image spectra have been evaluated from 512 x 512 pixel subscenes of image mode ERS-1 SAR scenes off Goa, Visakhapatnam, Paradeep and Portugal. The two recently acquired scenes off Portugal showed the signature of swell of wavelength ≈ 200m and internal waves of wavelength > 400m. Only internal waves of wavelength > 400m were seen in the scene off Goa observed on 11 March 1992. The scenes off Visakhapatnam and Paradeep did not show any wave like features, the latter appearing to be of “white noise” nature. There exists a 180° ambiguity in wave direction observed from radar imageries. Based on the method of Atanassov et al (1985), a computer program has been developed for the removal of the 180° ambiguity by using two images of the same area separated by a time interval which is small compared to the period of the dominant waves. The computer program has been successfully tested with computer simulated images.  相似文献   

5.
X波段测波雷达海流信息的提取决定着有效浪高结果的准确度。因此,对可能影响X波段测波雷达海流信息提取的各种环境因素以及雷达工作模式等进行了海浪回波成像仿真,然后采用目前测波雷达通用的算法对仿真回波图像进行了海流信息反演。主要研究了海表面风速、雷达天线架设距离海平面高度、天线转速、海流流速、海流流向与海浪方向夹角、所选取的图像帧数以及每帧图像大小对海流信息反演的影响。对比分析设定值与反演结果,可知海表面风速在6~14 m/s之间,天线高度大于20 m并且转速为50~70 r/min,流速小于200 cm/s并且主波浪向与流向夹角不接近90°,图像帧数为128帧并且每帧图像数据点数为128×128时,X波段测波雷达能获得最佳海流信息反演结果。  相似文献   

6.
Zhilin  Li  Guoxiang  Liu  Xiaoli  Ding 《The Photogrammetric Record》2006,21(114):124-140
This paper presents an attempt to explore the generation of digital elevation models (DEMs) by radargrammetry from same-side ERS-1/2 synthetic aperture radar (SAR) images. Two ERS-1 and two ERS-2 C-band (wavelength 5·6 cm) SAR images along parallel descending orbits, acquired in 1996 and 1997, are used to form four stereopairs. The test area is western Hong Kong which is dominated by mountains/hills that are largely covered by evergreen-broadleaf trees. The stereopairs covering the same area but with different time intervals (varying from 16 days to 1·5 years) have an intersection angle of 4·5° and a relatively small overlap of 30% (30 km). In addition to the effect of topography, the effect of temporal correlation on the accuracy of the resulting DEMs is also analysed for the first time. From the experimental results obtained in this study, the following conclusions may be drawn: (a) with same-side ERS-1/2 SAR images, an accuracy of 30 to 35 m is achievable; (b) the accuracy of a resulting DEM degrades almost linearly with an increase in slope when the terrain slope is below 30°, and in the areas with slope over 30°, the accuracy of the DEM is significantly degraded and even becomes unacceptable; (c) the worst accuracy is obtained in the foreslope directions and the best accuracy is obtained in the backslope directions; (d) the time interval between two SAR images has no significant effect on the accuracy of the DEM in general; (e) the time interval between two SAR images has no significant effect on the reliability of image matching.  相似文献   

7.
海洋雷达后向散射回波主要来自短重力波的Bragg 散射,这种散射与海面风场信息、边界层涡旋等密切相关。因此,可以从雷达散射截面反演风场信息。对1994 年4 月航天飞机成像雷达(SIRC/XSAR)获取的南中国海合成孔径雷达(SAR) 图像进行了分析研究。利用SIRC 数据,从SAR 图像谱提取了风向;根据CMOD4 模型,从C波段雷达后向散射系数反演风速;利用双尺度散射模型对反演的风速进行了对比分析。结果表明,从SIRC雷达数据可以反演海面风矢量,星载SAR是提取海面风场信息的有效技术手段之一。  相似文献   

8.
SAR影像中海洋浮油膜特征分割的Level Set方法   总被引:1,自引:0,他引:1  
黄晓霞  李红旮  黄波 《遥感学报》2005,9(5):549-554
介绍了一种全新的区域影像分割技术--基于迎风格式偏微分方程(PDE)的Level Set方法进行海洋浮油膜特征提取.在该方法中,海洋浮油膜特征表示为扩散界面,影像灰度的梯度决定了界面扩散的方向和强度.界面边缘在影像灰度差异动力和曲率流的共同作用下不断向外扩散,能够有效地克服尖锐突起和裂缝等,在特征边缘趋于稳定和光滑.同时,该方法对高噪声具有一定抑制作用,适用于低对比度高噪声图像,特别是SAR图象中特征提取.以不同地区ERS-2 SAR图像中海洋浮油膜提取为例,进行方法验证,同时对传统的影像分割技术进行对比.  相似文献   

9.
为了实现SAR图像区域网平差时连接点的自动稳健提取,面向相同侧视方向、近似平行轨道的异轨SAR图像,针对其方位向相对几何畸变较小、距离向相对几何畸变较大的特点,提出一种采用差异化约束的SAR图像连接点提取方法。该方法在构建SAR图像影像金字塔的基础上,采用增大方位向边长的长方形匹配窗口由金字塔顶层向下逐层进行相关系数匹配,利用方位向强约束、距离向弱约束的差异化随机采样一致性算法剔除误匹配点,并利用方位向全局双线性变换模型与距离向局部双线性变换模型进行下层金字塔影像的匹配点位预测。采用Envisat ASAR图像和国产机载SAR图像分别进行了连接点提取试验,验证了本文方法的有效性。  相似文献   

10.
干涉雷达永久散射体自动探测--算法与实验结果   总被引:9,自引:4,他引:5  
基于理论与模拟实验分析,提出并实现“双重阈值”PS自动探测算法,即时序相关系数阈值法和振幅离差指数阈值法相结合,达到PS自动探测时间效率与可靠性的统一。选用覆盖上海地区的26幅ERS-1/2 C波段SAR图像(1992~2002年),双重阈值PS探测算法得到了检验,实验结果表明,该方法能够有效地提取可靠的PS目标。  相似文献   

11.
雷达干涉测量(InSAR)和雷达立体测量(Radargrammetry)是使用SAR影像生成DEM的两种主动遥感新技术,前者利用反射雷达波的相位信息,而后者利用其灰度信息。本文利用ERS-1/2卫星对香港地区成像获取的SAR影像分别构成干涉像对和立体像对生成了DEM,并以外部DEM为参考,利用对比和统计方法分析了两种测量方法的精度情况和技术优势。  相似文献   

12.
利用SAR图像计算内波深度和振幅的可行性研究   总被引:9,自引:1,他引:9  
根据星载合成孔径雷达(SAR)内波成像机理,建立了包括KdV方程、作用量谱平衡方程和Bragg散射模型在内的内波深度和振幅探测模型,更为严谨地推导出用SAR图像计算内波深度的方法,并首次推导出内波振幅的计算方法.利用该方法对台湾东北部海域的两幅ERS-1 SAR内波图像进行了实例研究,结果表明,该方法是合理且可行的.  相似文献   

13.
Interferometric Synthetic Aperture Radar (InSAR), nowadays, is a precise technique for monitoring and detecting ground deformation at a millimetric level over large areas using multi-temporal SAR images. Persistent Scatterer Interferometric SAR (PSInSAR), an advanced version of InSAR, is an effective tool for measuring ground deformation using temporally stable reference points or persistent scatterers. We have applied both PSInSAR and Small Baseline Subset (SBAS) methods, based on the spatial correlation of interferometric phase, to estimate the ground deformation and time-series analysis. In this study, we select Las Vegas, Nevada, USA as our test area to detect the ground deformation along satellite line-of-sight (LOS) during November 1992–September 2000 using 44 C-band SAR images of the European Remote Sensing (ERS-1 and ERS-2) satellites. We observe the ground displacement rate of Las Vegas is in the range of ?19 to 8 mm/year in the same period. We also cross-compare PSInSAR and SBAS using mean LOS velocity and time-series. The comparison shows a correlation coefficient of 0.9467 in the case of mean LOS velocity. Along this study, we validate the ground deformation results from the satellite with the ground water depth of Las Vegas using time-series analysis, and the InSAR measurements show similar patterns with ground water data.  相似文献   

14.
基于仿真修正的序列SAR图像内波参数反演方法   总被引:2,自引:0,他引:2  
针对合成孔径雷达(Synthetic Aperture Radar,SAR)序列图像,提出了基于仿真修正的序列SAR图像内波参数反演方法。该方法使用规则化长波方程(Regular Long Wave,RLW)和M4S模型数值仿真SAR序列图像中的同一列内波,并通过与实际图像的对比修正反演参数。实验表明,该方法克服了现有方法依赖于历史水文数据精度和SAR成像条件的限制,其反演结果与实测值十分接近。  相似文献   

15.
The DEM of the Bhuj earthquake affected area of 50 x 50 km was generated using the ERS-1/2 SAR tandem data (May 15—16,1996). Region growing algorithm coupled with path following approach was used for phase unwrapping. Phase to height conversion was done using D-GPS control points. Geocoding was done using GAMMA software. A sample data of DEM of Shuttle Radar Topography Mission (SRTM) of the Bhuj area is made available by DLR Germany. The intensity image, DEM and Error map are well registered. The spatial resolution of this DEM is about 25 m with height accuracy of a few meters. The DEM derived through ERS SAR data is prone to atmospheric affects as the required two images are acquired in different timings where as SRTM acquired the two images simultaneously. An RMS height error of 12.06 m is observed with reference to SRTM though some of the individual locations differ by as much as 35 m.  相似文献   

16.
Mini SAR遥感系统,用微小型SAR做传感器,通过小型飞机或无人机为遥感平台获取地物信息,但载机平台在空中易受气流影响而偏离预设航线产生运动误差。文中首先分析载机平台运动特点,介绍系统中IMU/GPS组合导航数据预处理过程,论述载机平台转动误差、速度误差对SAR成像距离模型的影响。MiniSAR遥感系统获取的影像清晰,可用于制作正射影像图、基础地理信息库更新、灾害监测应急等领域,但不足之处在于影像中某些金属目标出现方位散焦现象。  相似文献   

17.
根据L/C双频共面SAR能够获取同一海域双波段电磁波后向散射系数,得到更多海洋目标特征信息的电磁散射特点,结合地球物理模型函数研究了一种新的SAR海面风场反演方法。利用L/C双频共面SAR的L和C两个波段的地球物理模型函数和后向散射系数等信息,通过地球物理模型函数联立以及构建和求解最小代价函数,直接从SAR数据本身获取海面风场信息,并借助辅助数据去除了风向的180°模糊,从而实现海面风场反演。仿真分析和海上机载同步飞行试验的研究结果表明,该方法可直接利用SAR数据本身获取精度较高的海面风速、风向;绝对辐射定标精度是决定海面风场反演精度的关键因素,海面风场反演误差随定标精度提高而减小;随着海面风速的增大,风速反演误差逐渐增大。论文提出的双频共面SAR海面风场反演方法解决了传统单波段单极化SAR海面风场反演存在的固有问题,机载同步飞行试验的海面风速和风向反演结果与调查船观测值的均方根误差分别为0.93 m/s和19.39°,可为星载SAR海面风场反演业务化和载荷研制提供支持。  相似文献   

18.
一种基于曲线SAR的三维目标特征提取与自聚焦新算法   总被引:5,自引:0,他引:5  
曲线合成孔径雷达(Curvilinear Synthetic Aperture Radar,简称曲线SAR)是一种新的三维成像模式,通过让载机作曲线飞行,曲线SAR系统能同时在方位维和高度维形成大的合成孔径。本文提出一种曲线SAR的三维目标特征提取和自聚焦新方法。新方法是建立在一种灵活的接收数据模型之上的参数化的新方法。仿真实验证明了所提方法的有效性。  相似文献   

19.
星载SAR复数图像的配准   总被引:16,自引:4,他引:16  
星载干涉雷达测量已经被证实用于生成大范围(乃至全球)的DEM或监测地表位移具有广阔的应用前景,其中SAR复数图像序列的精确配准是保证生成有效干涉相位图的重要环节之一。本文分析了卫星InSAR系统中所涉及的几种坐标系统变换问题,并提出了基于此的几何配准方案,即基于卫星轨道状态矢量、SAR成像几何进行配准的算法;同时,还设计了基于几何配准结果和能量影像相关技术的配准算法,最后使用ERS-1/2、JERS-1和RADARSAT卫星获取的3种SAR复数图像对分别做几何配准和相关配准试验和比较,并对卫星SAR图像质量和轨道数据质量作了定性分析。  相似文献   

20.
利用SAR影像配准偏移量提取地表形变的方法与误差分析   总被引:1,自引:1,他引:0  
陈强  罗容  杨莹辉  雍琦 《测绘学报》2015,44(3):301-308
单一的InSAR观测技术可提取地表沿雷达视线方向(LOS)上的一维位移,而利用SAR影像配准过程中的同名像素偏移量可提取地表沿雷达方位向(近南北向)与距离向(近东西向)的二维形变场,与LOS方向的一维形变形成优势互补。本文在分析SAR影像配准偏移量提取地表形变场方法的基础上,推导建立了雷达方位向与距离向形变提取的误差模型,探讨了该方法提取地表形变的主要误差源。以Bam地震ASAR影像和玉树地震PALSAR影像为数据源,分别开展同震形变场的提取与误差分析试验,结果表明,基于SAR像素配准偏移量提取同震形变场的精度主要受匹配窗口尺寸与过采样因子影响,形变提取误差随匹配计算窗口的增大而减小,形变提取精度随过采样因子的增大有适量提高,地形起伏效应在高差较大的SAR影像区域中表现较为显著。  相似文献   

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