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本文着重介绍全晶体管化X波段地面散射计的设计、结构与性能指标。This article describes design construction and characterization of a transistorized X-band ground-based scatterometer.

给出了一种改进的场方式反演方法，利用该方法从卫星散射计测量的后向散射强度的数据中唯一反演出大尺度海洋风场。We introduce a modified model approach to estimate the unique synoptic oceanic wind field from backscatter of spaceborne scatterometer.

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给出了一种改进的场方式反演方法，利用该方法从卫星散射计测量的后向散射强度的资料中唯一反演出大尺度海洋风场。We introduce a modified model approach to estimate the unique synoptic oceanic wind field from backscatter of spaceborne scatterometer.

本文给出了一种改进的场方式反演方法，利用该方法从卫星散射计测量的后向散射强度的数据中唯一反演出大尺度海洋风场。It is introduced that a modify model-based approach to estimating the unique synoptic oceanic wind field from backscatter of spaceborne scatterometer.

从结果可以看到，所采用的改进的场方式反演方法对模拟数据或真实散射计探测海面风场的反演是成功的。It is demonstrated very successfully that the simulated or real scatterometer data with the modified model estimation has been retrieved in this paper.

介绍神舟4号多模态微波遥感器散射计分系统的研制情况和在轨实验情况。We introduce in this paper the Scatterometer mode of Multimode Microwave Sensors on board Chinese Shenzhou-4 unmanned spacecraft launched on Dec. 29, 2002.

详细描述了地面特征参数的测量以及地物电磁散射特性实验测量过程和散射计测量原理。Measurements of the characteristic parameters of the ground, experimental measurement process and the principle of scatterometer measurement are described particularly.

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本文主要探讨用微波地面散射计测量地物散射系数方法，还讨论了散射计的有效照射面积的计算方法。A method for measurment of terrain scattering coefficient is presented. In addition, a calculable method of effective illumination area for microwave scatterometer is discussed.

虽然微波散射计具有全天候工作特点，但是大气衰减对散射计测量的后向散射系数仍然有影响。Though scatterometer is designed to acquire measurements of sea-surface winds under all weather conditions, the atmospheric attenuation still has influence on the measured NRCS.

通过仿真模型建立、分辨面元提取与风矢量模糊解消除，分析了散射计地面与星载定标特性，给出了散射计工作特性仿真结果。The resolution cell extraction method and the wind vector ambiguous solution are presented. The ground and space flight calibrating and scatterometer working characteristics are analyzed.

散射计和辐射计数据具有较大的空间覆盖和快速重访率，这使其成为联系监测南极冰盖的极好工具。Scatterometer and radiometer image data have a greater spatial and more frequent coverage, albeit at a lower spatial resolution, making these instruments ideal for monitoring the Antarctic ice sheet.