摘要
在光学遥感数据的应用过程中,地表太阳辐照度的量化问题对于遥感数据的获取和地表地物特性的反演等工作都是一个非常重要的环节,而地表太阳辐照度的定量计算又依赖于辐射源、目标物和传感器三者之间的几何关系以及目标地物的地表特征。利用山区地表太阳辐照度的计算模型,对不同时间、不同山区地形下的地表太阳辐照度进行了定量模拟,用三维图的方式分析了地表太阳辐照度随时间、地形坡度、坡向的变化规律,为光学遥感中地表太阳辐照度随时空变化的量化关系分析提供了更直观的依据。
In the application of the remote sensing data,the quantity of surface irradiance is very important in the acquisition of remote sensing data and retrieval of surface character,but the quantity of surface irradiance is based on the geometrical relationship of light source,objects,sensor and the surface character of objects.Based on the model of terrain surface irradiance,the terrain surface irradiance with different temporal and spatial distribution was quantitatively simulated.The law between the surface irradiance and the time,slope,aspect was showed with a 3-D coordinate,which provided a more direct basis for the quantity relationship of the surface irradiance and temporal and spatial distribution in the remote sensing.
出处
《武汉大学学报(信息科学版)》
EI
CSCD
北大核心
2011年第7期793-796,共4页
Geomatics and Information Science of Wuhan University
基金
国防预研资助项目(9140A03040408zk0901)
中国科学院通用光学定标与表征技术重点实验室开放研究基金资助项目
关键词
辐照度
坡度
坡向
光学遥感
6S
irradiance
slope
aspect
optical remote sensing
6S