首页|不同偏移量追踪算法提取冰川流速的亚像素级精度比较

不同偏移量追踪算法提取冰川流速的亚像素级精度比较

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偏移量追踪技术不易失相关,是利用光学与SAR卫星影像监测冰川流速的主要手段。该技术通过互相关方法获得像素级偏移量,并通过插值算法达到亚像素级别。实地测量冰川流速不易获取,难以用于验证亚像素级算法精度,因此本文采用图像处理方法对其精度进行分析。本研究以格陵兰Petermann和Kangerlussuaq冰川为例,通过模拟实验设定偏移量场并生成模拟的偏移影像,将COSI-Corr、autoRIFT和ImGRAFT等偏移量追踪软件得到的结果与设定偏移量场对比,而后使用三次函数拟合判断是否存在系统误差,并通过拟合函数的反函数对其进行校正。结果表明COSI-Corr软件的偏移结果的亚像素级系统误差较小,而autoRIFT和ImGRAFT存在一定的亚像素级系统误差且与实验区无关。autoRIFT的亚像素级系统偏差最大,校正后其单方向RMSE平均提升了0。0054pixels(px),提升率约为11%;而ImGRAFT(CCF-O)和ImGRAFT(NCC)的单方向RMSE平均分别提升了0。0014px和0。0012px,提升率较小。经校正后,autoRIFT精度最优,Petermann和Kangerlussuaq冰川区域的单方向综合精度分别为0。04px和0。12px;ImGRAFT(CCF-O)表现次之,不同实验条件下的单方向精度约为0。08px;ImGRAFT(NCC)较差,Petermann和Kangerlussuaq冰川区域的单方向综合精度分别约为0。09px和0。12px。
Precision comparison of different offset-tracking methods at sub-pixel level for glacier velocity study
Optical and/or SAR remote sensing images are frequently used to obtain glacier velocity fields through the use of offset tracking due to its strong decorrelation. Correlation algorithms extract the pixel-level offset,which can then be refined to a sub-pixel level through various interpolation techniques. However,the ac-curacy of these interpolation algorithms incorporated in different offset tracking software has rarely been assessed or compared. The lack of in-situ observations to confirm the sub-pixel precision of derived offset led to the aim of this study,which is to use a digital image processing method to evaluate the precision for various software and algorithms. Furthermore,the study suggests an algorithm to correct the possible offset tracking bias at the sub-pixel level. This study uses six pairs of Sentinel-2 images that observed two of the largest glaciers in Greenland,Petermann Glacier and Kangerlussuaq Glacier. These two glaciers account for roughly 4% each of the entire ice sheet's glacier mass loss and flow in northwestern and southeastern directions,respectively. The study com-bines the offset tracking results obtained from different algorithms,including COSI-Corr,autoRIFT,and Im-GRAFT (CCF-O and NCC),and treats them as pre-set offset fields. Using the Sinc interpolation,which is an optimal interpolation method according to the sampling theory,simulated offset images are generated using the pre-set offset fields and pre-event images. Performing the mentioned software and algorithms,offset tracking re-sults are obtained based on the pre-event images and simulated offset images. As all the algorithms first establish an offset value at the pixel level and then interpolate to the sub-pixel level,presuming the former being more de-pendable,this research assesses the precision and inspects possible bias at the sub-pixel level only. The displace-ment results obtained and the pre-set offset fields are wrapped to a range of[-0.5,0.5]and designated as y and x. A cubic function,y=ax+4(1-a)x3 (where a is the correction parameter),is chosen for the regression. The precision is exhibited by the fitting's RMSE,while parameter a indicates the presence of bias;if a equals 1,then no bias exists,but if it's not,there is a bias. Tthe inverse function of the fitting can rectify potential system-atic errors at the sub-pixel level. According to the regression results,the sub-pixel systematic error of COSI-Corr is negligible and can be disregarded,whereas autoRIFT and ImGRAFT (CCF-O or NCC) display a certain degree of systematic errors in their offset results. Specifically,the values of a are 1.008,0.778,0.915,and 0.886 for COSI-Corr,autoRIFT,ImGRAFT(CCF-O),and ImGRAFT(NCC),respectively. In COSI-Corr,Sinc function is used to interpolate the correlation coefficient matrix,while ImGRAFT applies bicubic interpola-tion regardless of the correlation algorithm being CCF-O or NCC. autoRIFT utilizes a rapid Gaussian pyramid upsampling algorithm for estimating the sub-pixel displacement with a precision of 1/64 pixel. After systematic error correction,the autoRIFT algorithm's RMSE decreased by an average of 0.0054 pixels in a single direc-tion,resulting in the most significant improvement among all algorithms and an 11% increase in precision. This demonstrates the significance of performing sub-pixel systematic error correction. On the other hand,the RMSE of ImGRAFT (CCF-O) and ImGRAFT (NCC) reduced slightly by an average of 0.0014 and 0.0012 pixels in a single direction,respectively. Whether to apply this correction to ImGRAFT depends on the desired level of pre-cision,as it results in only a 1.5% increase. Furthermore,as no noticeable systematic sub-pixel errors were de-tected,it is unnecessary to apply this correction to COSI-Corr. The regression results of all software/algorithms are similar across different study sites and/or deformation directions,indicating that sub-pixel systematic error is solely dependent on interpolation algorithm. After the systematic correction,all algorithms show reliable re-sults. COSI-Corr and autoRIFT show higher precision than ImGRAFT,with RMSEs of 0.04~0.14 pixels at Kangerlussuaq. Conversely,ImGRAFT shows slightly lower precision with RMSEs of 0.08~0.10 pixels at Pe-termann and 0.09~0.13 pixels at Kangerlussuaq. ImGRAFT (CCF-O) shows slightly better precision than Im-GRAFT (NCC). Given the much higher computational requirements of autoRIFT relative to the other algo-rithms,this study recommends combining autoRIFT with a post-correction step for systematic error.

offset trackingCOSI-CorrautoRIFTImGRAFTprecision of interpolationglacier velocity

杨治斌、李刚、毛燕婷、冯小蔓、陈卓奇

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中山大学测绘科学与技术学院南方海洋科学与工程广东省实验室(珠海),广东 珠海 519082

极地环境立体观测与应用教育部重点实验室(中山大学),广东 珠海 519082

偏移量追踪法 COSI-Corr autoRIFT ImGRAFT 插值精度 冰川流速

国家重点研发计划项目广东省基础与应用基础研究基金项目国家自然科学基金项目南方海洋科学与工程广东省实验室(珠海)创新团队建设项目

2021YFC28013002021B151502003242371136311021008

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(3)
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