Author_Institution :
P.Q. Res., Los Altos Hills, CA, USA
Abstract :
The conventional decomposition from a distributed target is to seek a solution of average single target MT, which preserves symmetry parameters A0, C, and D and a part which consists solely of non-symmetric parameters B0T-BT, ET, and FT. These parameters with index T are determined easily from four equations. The novel feature is to create a variable A0T in addition to the four non-symmetric target parameters of the old scheme. The new variable A0N extracts out of the general symmetry-preserving A0 a special target variable A0T, such that A0=A0T+A0N. The A0T now becomes part of the average single target parameters: A0T, B0T, BT, C, D, ET, FT, G, and H. In this scheme C, D, G, and H, the target symmetry and coupling parameters, are still preserved intact. What is new in the scheme is A0T which before was A0, "the generator and preservator of target symmetry". It is kind of ironic that the "symmetry-preserving" generator A0 itself is not preserved in the new scheme, but is split into A0T and A0N! That was why this new decomposition took so long in coming to development. The physical interpretation of the new scheme is a decomposition of the distributed target into a single average target MT and an N-target (N here standing for non-symmetry) and a background cloud of spherical particles. The C, D, G, and H still are preserved intact but the symmetry generator A0 is split, one part A0T contributing to the average single target MT and one new part A0N (N stands for new here!) forms a background cloud of elementary spheres. An example is shown consisting of a cloud of dipoles being averaged into a single dipole, a non-symmetrical N-target, and a new background cloud of elementary spheres, determined by A0N.
Keywords :
S-matrix theory; backscatter; geophysical techniques; radar applications; radar cross-sections; radar polarimetry; radar theory; remote sensing by radar; S-matrix; backscatter theory; distributed target; elementary sphere; extended target decomposition scheme; geophysical measurement technique; land surface terrain mapping; nonsymmetric parameters; radar remote sensing; radar scattering; special target variable; spherical particle; symmetry parameters; Ammeters; Art; Clouds; Ear; Equations; Linear matrix inequalities; Matrix decomposition; Polarization; Radar; Samarium;
Conference_Titel :
Geoscience and Remote Sensing Symposium, 1994. IGARSS '94. Surface and Atmospheric Remote Sensing: Technologies, Data Analysis and Interpretation., International