首页> 外文会议>Geoscience and Remote Sensing Symposium, 2004. IGARSS '04. Proceedings. 2004 IEEE International >Measurement of scattering coefficient dependence on soil moisture content and surface roughness by 35 GHz polarimetric scatterometer
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Measurement of scattering coefficient dependence on soil moisture content and surface roughness by 35 GHz polarimetric scatterometer

机译:用35 GHz极化散射仪测量散射系数对土壤水分含量和表面粗糙度的依赖性

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Polarimetric measurements of scattering coefficient /spl sigma//sup 0/ of a bare soil were performed changing a roughness of a soil surface and a soil moisture content using the 35 GHz polarimetric scatterometer. At Ka band, a few experimental results of /spl sigma//sup 0/ data are available. One of the purpose of this experiment is to obtain the surface backscattering characteristics to evaluate surface clutter interference with precipitation measurement from space using the Dual frequency Precipitation Radar (DPR, 13.8 GHz and 35.5 GHz), which is planned to be onboard the Global Precipitation Measurement (GPM) Mission core satellite to observe precipitation globally. In evaluation of surface clutter interference, /spl sigma//sup 0/ data for various surface conditions are needed, especially /spl sigma//sup 0/ dependence on soil moisture content and surface roughness. Another purpose of this experiment is to apply the measured /spl sigma//sup 0/ data to estimate a soil moisture content globally after the launch of the GPM core satellite. An angular scan range of the DPR is from nadir direction though the incidence angle of 8.4 degrees (with the 35.5 GHz radar) or 17 degrees (with 13.6 GHz radar), so the measured data by the DPR is useful to observe the earth surface condition globally. In this study, the roughness of the soil surface was measured with a laser profile meter to determine the roughness dependence of the scattering coefficient. A soil moisture content was measured comparing the weight of the soil before and after the heating of the soil. The soil was heated enough to contain no water. To increase the number of the independent samples for each experimental conditions (soil moisture content/surface roughness/incidence angle), azimuthal angle is changed like clockwork using the turntable of 2 m diameter. The system of the scatterometer is network analyzer based polarimeter.
机译:使用35 GHz极化散射仪,通过改变土壤表面粗糙度和土壤水分含量,对裸土的散射系数/ spl sigma // sup 0 /进行极化测量。在Ka频段,可获得/ spl sigma // sup 0 /数据的一些实验结果。该实验的目的之一是获得表面反向散射特性,以评估使用双频降水雷达(DPR,13.8 GHz和35.5 GHz)从太空进行的降水测量对地面杂波干扰的影响,该雷达计划在全球降水测量中使用(GPM)任务核心卫星用于观测全球降水。在评估表面杂波干扰时,需要/ spl sigma // sup 0 /各种表面条件的数据,尤其是/ spl sigma // sup 0 /取决于土壤水分含量和表面粗糙度。该实验的另一个目的是应用测量的/ spl sigma // sup 0 /数据来估计GPM核心卫星发射后的全球土壤水分含量。 DPR的角度扫描范围是从天底方向开始,虽然入射角为8.4度(使用35.5 GHz雷达)或17度(使用13.6 GHz雷达),所以DPR的测量数据对于观察地表状况非常有用全球范围。在这项研究中,用激光轮廓仪测量土壤表面的粗糙度,以确定散射系数的粗糙度依赖性。通过比较加热土壤之前和之后的土壤重量来测量土壤含水量。土壤被加热到不含水。为了增加每种实验条件(土壤水分含量/表面粗糙度/入射角)的独立样本数量,使用2 m直径的转盘像钟表一样更改方位角。散射仪的系统是基于网络分析仪的旋光仪。

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