基于Radarsat 2影像与地面数据的山地草甸土壤水分时空动态研究

C. Notarnicola, L. Pasolli, G. Cuozzo, F. Greifeneder, G. Bertoldi, S. Chiesa, G. Niedrist, Davide Castelletti, U. Tappeiner, L. Bruzzone, M. Zebisch
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引用次数: 1

摘要

在山区,土壤湿度是农业管理和自然灾害支持的关键参数。本文以山区为研究对象,提出了一种利用不同卫星传感器反演土壤水分的方法。对2010-2011年RADARSAT2四极化模式和Envisat ASAR宽幅带模式在VV偏振下获取的意大利德蒂罗尔省/上阿迪杰省上空图像进行了实验分析。土壤湿度的反演方法是基于支持向量回归(SVR)方法,该方法经过专门训练,能够考虑山区的地形效应。与实地活动期间收集的地面测量结果的比较表明,RMSE值约为SMC%的5%,而与固定地面站的比较报告的误差约为SMC%的9%。比较RADARSAT2和ASAR的SMC,两个数据集的SMC值分布非常相似。两个数据集的累积直方图曲线显示ASAR产品中SMC的略微低估。这可以归因于ASAR WS分辨率的降低和VV偏振的使用。
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Temporal and spatial soil moisture dynamics in mountain meadows by integrating Radarsat 2 images and ground data
In mountain areas, soil moisture is a key parameter for both agricultural management and natural hazard support. This paper presents an approach for retrieval of soil moisture content (SMC) from different satellite sensors with a specific focus on mountain areas. The experimental analysis was carried out on images acquired over the Südtirol/Alto Adige Province (Italy) during 2010-2011 from the RADARSAT2 in quad-pol mode and Envisat ASAR in Wide Swath mode in VV polarization. The methodology for soil moisture retrieval is based on the Support Vector Regression (SVR) method specifically trained to be able to consider topographic effects of the mountain areas. The comparison with ground measurements collected during field campaigns indicates an RMSE value of around 5% of SMC% while the comparison with fixed ground stations reports an error of around 9% of SMC%. Comparing RADARSAT2 and ASAR SMC, both datasets reveal very similar distributions of SMC values. The cumulative histogram curve for the two datasets shows a slight underestimation of SMC in the ASAR product. This could be ascribed to the reduced resolution of ASAR WS and the use of VV polarization.
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