One danger or threat to an aircraft is from weather that includes turbulent air. Sudden updrafts, downdrafts, or wind shears can inflict injury on occupants and damage to the aircraft, or cause the total loss of aircraft and passengers. Turbulent air itself cannot be accurately measured by radar at any significant range, but such turbulence generally is accompanied by rain, hail, or particulate matter that can be. At short ranges (currently approximately up to 40 nautical miles (nm) from the aircraft), airborne Doppler radar information can give a direct reading of the movement of airborne particles and, hence, a fairly direct measure of air turbulence and potential hazard. However, current practical airborne radars that are affordable and fit on commercial aircraft do not have the ability to measure Doppler effects much farther than this, giving too little reaction time for the pilots to plan effective and efficient routes around the hazard.
The present invention provides methods and systems for predicting turbulence over an extended range. An exemplary method includes decomposing radar reflectivity data into multiple adaptive three-dimensional Gaussian component functions and decomposing turbulence data into multiple adaptive three-dimensional Gaussian component functions.
The real measured turbulence data t(x,y,z) is shown in
The present invention provides adaptive signal decomposition and a neural network method to extend the weather radar turbulence prediction range from 40 nm to 320 nm (approximate radar limit). With the decomposed reflectivity and turbulence components as the input and output, a proposed backward propagation neural network learns the relationship between reflectivity and turbulence. The trained neural network then predicts the turbulence at an extended range where only reflectivity data are available. Advantageously, the adaptive signal decomposition method may be used for object tracking, such as, but not limited to, weather tracking, cloud tracking, bird flock tracking, aircraft tracking, etc.
Preferred and alternative embodiments of the present invention are described in detail below with reference to the following drawings:
Radar relies on a transmission of a pulse of electromagnetic energy, referred to herein as a signal. The antenna 56 narrowly focuses the transmission of the signal pulse. Like the light from a flashlight, this narrow signal illuminates any objects in its path and illuminated objects reflect the electromagnetic energy back to the antenna.
Reflectivity data correspond to that portion of a radar's signal reflected back to the radar by liquids (e.g., rain) and/or frozen droplets (e.g., hail, sleet, and/or snow) residing in a weather object, such as a cloud or storm, or residing in areas proximate to the cloud or storm generating the liquids and/or frozen droplets.
The radar controller 50 calculates the distance of the weather object relative to the antenna 56 based upon the length of time the transmitted signal pulse takes in the transition from the antenna 56 to the object and back to the antenna 56. The relationship between distance and time is linear as the velocity of the signal is constant, approximately the speed of light in a vacuum. Honeywell's® RDR-4000 airborne weather radar is an example weather radar that provides the radar reflectivity data and the short range Doppler radar information.
In one embodiment, the present invention includes turbulence prediction systems and methods using adaptive signal decomposition and a neural network's approach to forecast turbulence information beyond the 40 nm range. An exemplary method includes reflectivity signal decomposition and turbulence signal decomposition. The method decomposes the reflectivity data into multiple adaptive, three-dimensional Gaussian component functions, whose parameters, such as center position, amplitude, and dimensional standard deviations, are determined adaptively to maximally match the measured reflectivity. Performing the reflectivity signal decomposition includes using adaptive three-dimensional Gaussian base functions with unit energy. The turbulence data are decomposed into adaptive three-dimensional Gaussian base functions, with their parameters adjusted to maximally match the measured turbulence data.
With the decomposed reflectivity and turbulence components as input and output, backward propagation of the neural network is performed for learning the relationship between reflectivity and turbulence. The trained neural network is then used to predict the turbulence at an extended range where only reflectivity data are available. The adaptive signal decomposition method proposed herein may also be used for object tracking, e.g., weather/cloud tracking, bird flock tracking, aircraft tracking, etc.
The new coordinates after coordinate change are calculated as shown in
The rotation angle θ is calculated as shown in
The transform from new coordinates back to old coordinates is shown in
Adaptive Decomposition of Reflectivity: The following equations show the adaptive decomposition of reflectivity. The three-dimensional Gaussian base function is proposed, as shown in
which has unit energy, i.e., ∫∫∫f2(x′,y′,z′)dx′dy′dz′=1. Placing equation (1) into equation (4), the three-dimensional Gaussian base function in xyz coordinates is shown in
At initialization, the current reflectivity r1 is set to the measured reflectivity data r(x,y,z), i.e., shown in
The center position and dimensional deviations of the three-dimensional Gaussian base function are determined by solving the following optimization problem, where means inner product shown in
The amplitude of the Gaussian base function is calculated as shown in
The first reflectivity component function v1 is therefore shown in
Removing the first component function v1 from the original reflectivity data r1, a new reflectivity r2 data is attained, i.e., shown in
Repeating the above procedure for N iterations, there become N reflectivity component functions shown in
The real measured data r(x,y,z) is shown in
It is interesting to note that the residual of the adaptive decomposition is always bounded. For continuous signal r, the residual will be reduced to zero as the number of iterations N goes to infinity.
Ignoring the residual rN+1, the N component functions are used to approximate the reflectivity function as shown in
Adaptive Decomposition of Turbulence: The following equations show the adaptive decomposition of turbulence. The turbulence base function is proposed, as shown in
This turbulence base function also has unit energy, i.e., ∫∫∫p2(x′,y′,z′)dx′dy′dz′=1. Placing the equation of
At initialization, the measured turbulence data t(x,y,z) are assigned to the current turbulence t1, i.e., shown in
The parameters of the turbulence base function are determined by solving the following optimization problem shown in
The amplitude of the turbulence base function is calculated as shown in
The first turbulence component function u0 is shown in
Removing the first component function u1 from the original turbulence data t1, a new turbulence data t2 is attained, i.e., as shown in
Repeating the above procedure for M iterations, M component functions are shown in
Ignoring the residual tM+1, the M component functions are used to reconstruct the turbulence function as shown in
Beyond ˜40 nm, the weather radar can effectively measure only reflectivity. The measured reflectivity data is decomposed into reflectivity components (
While one embodiment of the invention has been illustrated and described, as noted above, many changes can be made without departing from the spirit and scope of the invention. For example, processors are used to automatically perform the steps shown and described in the flowcharts above. Accordingly, the scope of the invention is not limited by the disclosure of one embodiment. Instead, the invention should be determined entirely by reference to the claims that follow.
This application claims the benefit of U.S. Provisional Application Ser. Nos. 61/163,362 and 61/163,355 both filed Mar. 25, 2009, the contents of which are hereby incorporated by reference.
Number | Date | Country | |
---|---|---|---|
61163362 | Mar 2009 | US | |
61163355 | Mar 2009 | US |