首页> 外文期刊>International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences >ASSESSMENT OF RAINFALL INFLUENCE ON SENTINEL-1 TIME SERIES ON AMAZONIAN TROPICAL FORESTS AIMING DEFORESTATION DETECTION IMPROVEMENT
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ASSESSMENT OF RAINFALL INFLUENCE ON SENTINEL-1 TIME SERIES ON AMAZONIAN TROPICAL FORESTS AIMING DEFORESTATION DETECTION IMPROVEMENT

机译:对亚马逊热带森林瞄准森林检测改进的亚马逊热带森林的降雨影响评估

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This work aims to determinate the relationship between C-band SAR backscattering measurements over Amazonian tropical forests and hourly precipitation rates, and to study the feasibility of a SAR-anomaly masking method based on orbital rain measurements. To do so, a comprehensive dataset of ESA’s Sentinel-1 backscattering data and the concomitant GPM-IMERG precipitation data was collected and analysed. Backscattering anomalies were characterized in a statistically meaningful way. GAM models were then adjusted to the backscatter-rain data pairs. The computed models show a positive correlation between non-anomalous backscattering values and accumulated rain, of approximately 0,2 dB/mm·h−1 and 0,4 dB/mm·h−1 for VV and VH polarizations. Negative anomalies, which can easily mislead deforestation algorithms, have a strong negative correlation with rain rate observed at the time of the SAR acquisition. This is especially true for VV measurements. The subsequent anomaly masking procedure, based on computed accumulated and hourly rain thresholding, yielded unsatisfactory results. These poor results are probably due to the coarse resolution of the 0.1° GPM-IMERG data, which is insufficient to track anomaly-generating atmospheric events such as storm rain cells. Rain-related changes in SAR backscattering can compromise deforestation detection algorithms, and further research and sensor developing is needed to increase spatial resolution of precipitation measures, to reach an optimal backscattering anomaly screening.
机译:这项工作旨在确定C波段SAR对亚马逊热带森林和每小时降水率的影响的关系,并研究基于轨道雨量测量的SAR异常掩蔽方法的可行性。为此,收集并分析了ESA的Sentinel-1反向散射数据和伴随的GPM-IMERG降水数据的全面数据集。反向散射异常以统计上有意义的方式表征。然后将GAM模型调整到后散雨数据对。计算的模型显示出非异常的反向散射值与VV和VH偏振的累积雨之间的累积雨量和累积雨之间的正相关性,其为大约0.2dB / mm·H-1和0.4dB / mm·H-1。负异常,可以容易地误导遮瑕算法,在SAR采集时观察到的雨率具有强烈的负相关性。 VV测量尤其如此。基于计算的累计和每小时雨阈值的后续异常掩蔽程序产生了不令人满意的结果。这些差的结果可能是由于0.1°GPM-IMERR数据的粗糙分辨率,这不足以跟踪异常产生的大气事件,如暴雨细胞。与雨散射的雨水相关变化可以危及砍伐森林检测算法,并且需要进一步的研究和传感器开发来增加降水措施的空间分辨率,以达到最佳的反向散射异常筛选。

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