DocumentCode
2742864
Title
On the imaging of sea wave with coherent microwave radar
Author
Drake, D. ; Wright, John
Author_Institution
Naval Research Lab., Washington, D. C., USA
Volume
12
fYear
1974
fDate
27181
Firstpage
318
Lastpage
318
Abstract
An idealized, coherent radar traveling at a speed,
maps a scatterer at a range, R and position
parallel to the direction of travel and measured from the axis of radar look) into an imaged position.
where
is the component of scatterer velocity along the line of sight. Since the number of scatterers
, say, is conserved in this transformation.
Image patterns will thus be formed if either
or
varies significantly with
. The former case is analogous to ordinary incoherent optical imaging but the latter is uniquely coherent imaging. In a two scale model incoherent imaging of sea waves results from tilting of Bragg Scatterers by the large wave and by modulation of the Bragg wave amplitude through straining by the large wave. The tilting and straining effects have a similar dependence on large wave slope but the latter has a much different windspeed and Bragg wavenumber dependence. Since, in the two scale case,
is derived from the orbital velocity of the large wave it is quasi-periodic and can also produce a wave-line image by coherent imaging. We have recently examined a number of examples of coherent imagery of the sea for evidence of the above outlined mechanisms and find that we are able to isolate the characteristics of both coherent and incoherent type imagery.
maps a scatterer at a range, R and position
parallel to the direction of travel and measured from the axis of radar look) into an imaged position.
where
is the component of scatterer velocity along the line of sight. Since the number of scatterers
, say, is conserved in this transformation.
Image patterns will thus be formed if either
or
varies significantly with
. The former case is analogous to ordinary incoherent optical imaging but the latter is uniquely coherent imaging. In a two scale model incoherent imaging of sea waves results from tilting of Bragg Scatterers by the large wave and by modulation of the Bragg wave amplitude through straining by the large wave. The tilting and straining effects have a similar dependence on large wave slope but the latter has a much different windspeed and Bragg wavenumber dependence. Since, in the two scale case,
is derived from the orbital velocity of the large wave it is quasi-periodic and can also produce a wave-line image by coherent imaging. We have recently examined a number of examples of coherent imagery of the sea for evidence of the above outlined mechanisms and find that we are able to isolate the characteristics of both coherent and incoherent type imagery.Keywords
Extraterrestrial measurements; Microwave imaging; Optical imaging; Optical scattering; Position measurement; Radar imaging; Radar measurements; Radar scattering; Sea measurements; Velocity measurement;
fLanguage
English
Publisher
ieee
Conference_Titel
Antennas and Propagation Society International Symposium, 1974
Type
conf
DOI
10.1109/APS.1974.1147302
Filename
1147302
Link To Document