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71.
Mourad Lazri Soltane Ameur Yacine Mohia 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2014
In the present paper, an artificial neural network (ANN) based technique has been developed to estimate instantaneous rainfall by using brightness temperature from the IR sensors of SEVIRI radiometer, onboard Meteosat Second Generation (MSG) satellite. The study is carried out over north of Algeria. For estimation of rainfall, weight matrices of two ANNs namely MLP1 and MLP2 are developed. MLP1 is to identify raining or non-raining pixels. When rainy pixels are identified, then for those pixels, instantaneous rainfall is estimated by using MLP2. For identification of raining and non raining pixels, 7 input parameters from the IR sensors are utilized. Corresponding data of raining/non-raining pixels are taken from radar. For instantaneous rainfall estimation, 14 input parameters are utilized, where 7 parameters are information about raining pixels and 7 parameters are related with cloud features. The results obtained show the neural network performs reasonably well. 相似文献
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Sriram Saran Anup DasShiv Mohan Manab Chakraborty 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2014
The surface layer of the Moon preserves vital evidences of lunar impact and cratering processes due to the absence of any Aeolian and fluvial erosion processes acting on it. By examining these evidences, which are recorded throughout the evolutionary history of the Moon, several basic aspects of lunar science can be understood, and this has direct relevance to the surfaces of other airless bodies within the solar system. In this study, rock abundance data obtained from Thermal Infrared (TIR) observations and radar Circular Polarization Ratio (CPR) data sets obtained from polarimetric SAR observations were correlated at some sample sites on the lunar surface. Preliminary results yielded qualitative and quantitative estimates for surface rock abundances. Except at distal ejecta deposits of young, bright craters a general correlation was observed between the two datasets. Mixed results were observed from the impact melt flows where the situation is complex due to the possible subsurface-volume and volume-subsurface interactions of the radar waves. But the flow features were clearly separated from the interior and ejecta regions of their parent craters in terms of CPR and rock abundances. The extent and distributions of pyroclastic deposits and dark haloed regions could not be distinctly identified at the resolution of datasets utilized. Near Gerasimovich D crater, the Diviner Radiometer has provided the first TIR observations of a newly discovered impact melt flow which was not visible in the optical imagery. This facilitated the first ever quantitative comparisons of the radar CPR and rock abundance values near such a region. Also, significant differences in spatial patterns between the radar and rock concentration data sets were observed, owing to the differences in the sensitivity of the two observations. 相似文献
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Saurabh Das Ashish K. Shukla Animesh Maitra 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2010
The microstructure of rain has been studied with observations using a vertical looking Micro Rain Radar (MRR) at Ahmedabad (23.06°N, 72.62°E), a tropical location in the Indian region. The rain height, derived from the bright band signature of melting layer of radar reflectivity profile, is found to be variable between the heights 4600 m and 5200 m. The change in the nature of rain, classified on the basis of radar reflectivity, is also observed through the MRR. It has been found that there are three types of rain, namely, convective, mixed and stratiform rain, prevailing with different vertical rain microstructures, such as, Drop Size Distribution (DSD), mean drop size, rain rate, liquid water content and average fall speed of the drops at different heights. It is observed that the vertical DSD profile is more inhomogeneous for mixed and stratiform type rain than for convective type rain. It is also found that the large number of drops of size <0.5 mm is present in convective rain whereas in stratiform rain, drops concentration is appreciable up to 1 mm. A comparison of measurements taken by ground based Disdrometer and that from the 200 m level obtained from MRR shows good agreement for rain rate and DSD at smaller rain rate values. The results may be useful for understanding rain structures over this region. 相似文献
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多普勒调频率是SAR方位向压缩的关键参数之一. 调频率的失配会带来严重的方位向散焦, 从而影响成像质量. 基于减灾、防灾目的, 需要对SAR数据快速成像, 从而相应要求对多普勒调频率进行快速估计处理. 根据多普勒调频率快速估计需求, 提出了一种基于轨道参数法和Map Drift算法估计多普勒调频率的综合反演算法, 利用多普勒调频率与距离的关系, 简化整个估计流程, 从而提高估计速度. 同时给出了一种块数据筛选的方法, 用于选择综合反演法中所采用的块数据. 实验结果表明, 综合反演法能够在满足成像质量要求的基础上, 快速估计出多普勒调频率. 相似文献
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文章讨论了星载降水测量雷达(SPR)重频设计要求和约束条件,并以GPMKuPR系统参数为例,研究了SPR重频设计的约束条件,提出和分析了几种重频设计方案。仿真结果表明一种自适应重频技术完全满足系统要求,并能获得最多脉冲积累数。 相似文献
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叙述分析处理连续波(CW)信号的重要性,并介绍测定CW信号频率特征的方法。讨论了运行载体上的CW信号频率的调制特性和多普勒频移以及侦收系统噪声对测定信号频率的影响。 相似文献
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