海面风应力和海面阻力系数的星载SAR遥感测量

在海面张力波和短重力波星载合成孔径雷达(SAR)成像机理的基础上,建立了海面风应力和阻力系数的遥感测量模型.该模型由辐射定标模式、风速反演模式以及风应力和阻力系数计算模式3部分组成.同时以雷达卫星SAR为例,对海面阻力系数和风应力的遥感测量进行了探索性研究,获得了较好的结果.     

星载SAR遥感浅海水下地形的最佳海况模拟仿真

根据星载合成孔径雷达(SAR)浅海水下地形和水深成像机理,建立了浅海水下地形和水深雷达后向散射截面仿真模型,模拟了浅海水下地形的雷达后向散射截面,分析了流速、流向、风速和风向与SAR水下地形观测之间的关系.结果显示,流经水下地形的流速越大,水下地形越易被SAR观测到.流向与水下地形坡度方向平行(0°)是水下地形观测的最佳流向;流向与水下地形坡度方向垂直(90°)最不利于SAR对水下地形成像.星载SAR水下地形观测的最佳风速范围为3～9 m/s.风向对水下地形成像的影响比较复杂,30°～89°是最佳的风向范围.     

Retrieval of ocean surface wind stress and drag coefficient from spaceborne SAR

A model for retrieval of wind stress and drag coefficient on the sea surface with the data measured by spacebome synthetic aperture radar (SAR) has been developed based on the SAR imaging mechanisms of ocean surface capillary waves and short gravity waves. This model consists of radiometric calibration, wind speed retrieval and wind stress and drag coefficient calculation. A Radarsat SAR image has been used to calculate wind stress and drag coeffi cient. Good results have been achieved.