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Temporal and Spatial Soil Moisture Change Pattern Detection Using Multi-Temporal Radarsat SCANSAR Images

机译:利用多时相雷达SCANSAR图像检测时空土壤水分变化模式

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摘要

Monitoring soil moisture dynamics is very important for understanding soil-vegetation interactions in both space and time. The currently available satellites, however, are single polarization, single frequency sensors such as ERS-1/2, Radarsat, and JERS-1. There is a need to develop a technique to estimate soil moisture information from these available data sources at both regional and local scales. rnIn this study, we demonstrate a technique using the multi-temporal C band HH polarized Radarsat SCANSAR data to estimate the relative soil moisture change. The experiment data from SGP97 covered a whole range of vegetation growing season and different type agriculture fields. This technique is mainly involved two steps:1. derived from TM and AVHRR measurements for spatial and temporal variations of vegetation covers at different scales. Using a simple radiative transfer model for vegetation volume scattering and the Integral Equation Model (IEM) for surface scattering with the field in situ measurements as the input, we compared the simulated and SAR measured backscattering coefficients in different agricultural fields. We, then, parameterized a semi-empirical model for the different land surface cover types. This semi-empirical model was applied to minimize the effects of the vegetation volume scattering and extinction in radar measurements. 2. Radar incidence angle and surface roughness correction: To make radar incidence correction and eliminate the surface roughness effects, a wide range of surface parameters (soil moisture, surface RMS height, correlation length, incidence angle) was input to the IEM model to simulate the effect of surface roughness and radar incidence angle on the sensitivity of soil moisture to the radar backscattering coefficient. A simple model was established to simulate the effects of incidence angle and surface roughness. Inversion results show that for the C band HH polarized Radarsat SCANSAR data with a range of incidence angle from 20° to 40°, the soil moisture change value can be derived with an acceptable accuracy. The temporal and spatial soil moisture change patterns are associated with rainfall and vegetation cover, as well as the soil hydraulic characteristics.
机译:监测土壤水分动态对于了解时空上的土壤-植被相互作用非常重要。但是,当前可用的卫星是单极化,单频率传感器,例如ERS-1 / 2,Radarsat和JERS-1。需要开发一种技术来从区域和地方尺度的这些可用数据源中估算土壤湿度信息。在这项研究中,我们展示了一种使用多时相C波段HH极化Radarsat SCANSAR数据估算土壤相对湿度变化的技术。 SGP97的实验数据涵盖了整个植被生长期和不同类型的农业领域。该技术主要包括两个步骤:1。通过TM和AVHRR测量得出不同尺度上植被覆盖的时空变化。使用用于植被体积散射的简单辐射传递模型和用于表面散射的积分方程模型(IEM)(以现场测量为输入),我们比较了不同农业领域中模拟的和SAR测量的反向散射系数。然后,我们为不同的地表覆盖类型参数化了一个半经验模型。该半经验模型用于最小化雷达测量中植被体积散射和消光的影响。 2.雷达入射角和表面粗糙度校正:为了进行雷达入射角校正并消除表面粗糙度影响,将广泛的表面参数(土壤湿度,表面RMS高度,相关长度,入射角)输入IEM模型进行仿真表面粗糙度和雷达入射角对土壤水分对雷达后向散射系数敏感性的影响。建立了一个简单的模型来模拟入射角和表面粗糙度的影响。反演结果表明,对于入射角范围为20°至40°的C波段HH极化Radarsat SCANSAR数据,可以以可接受的精度得出土壤湿度变化值。土壤水分的时空变化模式与降雨和植被覆盖以及土壤水力特征有关。

著录项

  • 来源
  • 会议地点 Three Gorges Dam(CN);Three Gorges Dam(CN)
  • 作者单位

    Laboratory of Remote Sensing Information Sciences Insititute of Remote Sensing Applications, Chinese Academy of Sciences P.O. BOX 9178, Beijing, 100101, China. E-mail: Tiger@lab.irsa.ac.cn;

    Laboratory of Remote Sensing Information Sciences Insititute of Remote Sensing Applications, Chinese Academy of Sciences P.O. BOX 9178, Beijing, 100101, China;

    Laboratory of Remote Sensing Information Sciences Insititute of Remote Sensing Applications, Chinese Academy of Sciences P.O. BOX 9178, Beijing, 100101, China;

    Laboratory of Remote Sensing Information Sciences Insititute of Remote Sensing Applications, Chinese Academy of Sciences P.O. BOX 9178, Beijing, 100101, China;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 遥感技术的应用;水资源开发;
  • 关键词

  • 入库时间 2022-08-26 13:57:42

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