A terahertz photonic imaging radar system based on inverse synthetic aperture technique

2021 ◽  
Author(s):  
Shiwei Wang ◽  
Zijie Lu ◽  
Hongqi Zhang ◽  
Lu Zhang ◽  
Mengyao Qiao ◽  
...  
2017 ◽  
Vol 9 (6) ◽  
pp. 1339-1343 ◽  
Author(s):  
Simon Wagner ◽  
Joachim Ender

Air target recognition is a critical step in the radar processing chain and reliable features are necessary to make a decision. The number and position of jet engines are useful features to perform a pre-classification and give a list of possible targets. To extract these features, a sparse decomposition framework for inverse synthetic aperture radar (ISAR) images is presented. With this framework different components of the target can be detected, if signal models for these parts are available. To use it for the detection of jet engines, a review of a signal model for air intakes, which was developed by Borden, is given. This model is based on the common assumption that the propagation of electromagnetic waves inside jet engines has the same dispersive behavior as inside waveguides. With this model a decomposition of a real ISAR image, measured with the tracking and imaging radar system of Fraunhofer FHR, into point-like scattering centers and jet engines is presented.


Author(s):  
Ren Xiao-yuan Ren Xiao-yuan ◽  
Liu Hai-bo Liu Hai-bo ◽  
Li Jin-bing Li Jin-bing

1977 ◽  
Vol 82 (24) ◽  
pp. 3445-3451 ◽  
Author(s):  
David Atlas ◽  
Charles Elachi ◽  
Walter E. Brown

1996 ◽  
Vol 23 ◽  
pp. 209-216 ◽  
Author(s):  
Eric Rignot ◽  
Rick Forster ◽  
Bryan Isacks

The first topographic and ice-motion maps of the northwestern flank of Hielo Patagónico Norte (HPN, northern Patagonia Icefield), in Chile, were produced using satellite synthetic-aperture interferometric radar data acquired by NASA’s Spaceborne Imaging Radar C instrument in October 1994. The topographic map has a 10 m vertical precision with a 30 m horizontal spacing, which should be sufficient to serve as a reference for monitoring future mass changes of the icefield. The ice-motion map is accurate to within 4 mm d−1 (or 1 m a−1). The radar-derived surface topography and ice velocity are used to estimate the ice discharge from the accumulation area of four outlet glaciers, and the calving flux and mass balance of Glaciar San Rafael. The results demonstrate the use of SAR interferometry for monitoring glaciological parameters on a spatial and temporal scale unattainable by any other means.


1995 ◽  
Vol 33 (4) ◽  
pp. 817-828 ◽  
Author(s):  
E.R. Stofan ◽  
D.L. Evans ◽  
C. Schmullius ◽  
B. Holt ◽  
J.J. Plaut ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document