1.
Background
Scanning
radars and vertically-pointing profilers in operational use for meteorology
today utilize Doppler shift information to derive the radial (along-beam)
component of motion of the scatterers in the sensor's field of view.
That motion typically yields important (but incomplete) information
on the wind speed and/or fall velocities of the scatterers. However,
Doppler techniques also impose limitations on the measurements they
obtain - for example through the 'folding' or aliasing of Doppler
velocities - and this aliasing can seriously complicate the analysis
of radar data in complex atmospheric circulations. In addition, Doppler
techniques yield no measure of the component of velocity transverse
to the beam, which in most applications would prove extremely valuable.
The
limitations cited above in part motivate longstanding research in
the U.S. and elsewhere directed toward development of signal analysis
techniques that don't depend upon Doppler shift information. This
work has yielded a family of such techniques which generally make
use of the correlation function behavior of remotely sensed signals
as received at two or more closely spaced antennas (see Figure O1).
These techniques are able (with varying success) to derive estimates
of the component of scatterer velocity transverse to the radar beam.
RAP
scientists A. Praskovsky and E. Praskovskaya have conceived a new
approach to the analysis of spaced antenna measurements that utilizes
auto- and cross-structure functions to derive scatterer motion information.
That approach - termed the Structure Function Analysis
of Received Signals (UCAR-STARS) - utilizes the time
series of power measurements derived from a radar or other remote
sensor. In contrast, the spaced antenna methods that utilize correlation
function techniques generally rely upon the time series of both power
and phase information from the radar system.
