Method and apparatus for remote measurement of wind direction and speed in the atmosphere

• US 4,351,188 A
• Filed: 05/28/1981
• Issued: 09/28/1982
• Est. Priority Date: 05/30/1980
• Status: Expired due to Fees

• Current Assignee: Radio Research Laboratories Ministry of Posts & Telecommunications
• Original Assignee: Radio Research Laboratories Ministry of Posts & Telecommunications
• Inventors: Masuda, Yoshihisa, Fukushima, Madoka, Akita, Kin-ichiro
• Primary Examiner(s): Ciarlante, Anthony V.
• Assistant Examiner(s): Carlson, David V.
• Application Number:
  US06/268,107
• Time in Patent Office: 488 Days
• Field of Search: 343/5 W, 343/6 R, 73/189, 73/188, 73/170 R
• US Class Current: 73/170.13
• CPC Class Codes: G01S 13/86 Combinations of radar systems with non-radar systems, e.g. sonar, direction finder
• CPC Class Codes: G01S 13/951 ground based
• CPC Class Codes: G01S 15/885 Meteorological systems
• CPC Class Codes: Y02A 90/10 Information and communication technologies [ICT] supporting adaptation to climate change, e.g. for weather forecasting or climate simulation

Abstract

An acoustic wave source and a radio wave source are installed close to each other on the ground. When an acoustic wave pulse is transmitted vertically into the atmosphere by the acoustic wave source, spherical wavefronts formed in the atmosphere by the acoustic wave are propagated upwardly at the velocity of sound. When a continuous radio wave is transmitted from the radio wave source toward the spherical wavefronts, it is reflected by the wavefronts and the reflected radio waves are converged to form a focusing spot on the ground. The position where the spot due to the convergence of the reflected radio waves is formed with the maximum intensity is detected by means of an antenna network formed of a multiplicity of receiving antennas laid out in the pattern of a lattice. The time-course change of such positions of the spots is traced to realize remote measurement of the height distribution of wind direction and speed in the atmosphere under surveillance.

Claims

1. A method for the measurement of wind direction and speed at high altitudes in the atmosphere, comprising the steps of transmitting vertically into the atmosphere a pulse of acoustic waves from an acoustic wave source installed on the ground thereby causing the pulse of acoustic wave to produce spherical wavefronts, transmitting continuous radio waves from a radio wave source installed on the ground toward the spherical wavefronts thereby enabling the radio waves to be reflected by the spherical wavefronts, detecting the position of the reflected radio waves formed as a focusing spot on the ground, tracing the time-course change of the positions of maximum intensity of the focusing spot of the reflected radio waves, and calculating the height distribution of wind direction and speed in the atmospheric region based on the time-course change of the position of the focusing spot.

2. The method according to claim 1, wherein the detection of the positions of the reflected radio waves to converge to form the focusing spot on the ground is effected by an antenna network comprising a plurality of antennas laid out in the pattern of a lattice.

3. An apparatus for the measurement of wind direction and speed, comprising a pulse acoustic wave source for transmitting a pulse acoustic wave vertically into the atmosphere to propagate the acoustic wave to produce spherical wavefronts, a radio wave source for transmitting a continuous radio wave in the direction of the spherical wavefronts, a receiving antenna network formed of a plurality of receiving antennas laid out in the pattern of a lattice, said receiving antenna network being disposed downwind of said pulse accoustic wave source and said radio wave source and adapted to detect the radio wave reflected by the spherical wavefronts, radio wave receivers connected one each of said receiving antennas of the antenna network, means for detecting the antenna receiving the reflected radio wave of the maximum intensity from among the antennas of the antenna network, and means for calculating the wind direction and speed based on the position of the antenna receiving the reflected radio waves of the maximum intensity.

4. The apparatus according to claim 3, which further comprises means for displaying the wind direction and speed determined by said calculating means.

5. The apparatus according to claim 3, wherein the radio waves are transmitted toward the spherical wavefronts at a wavelength such that, at the time that the waves perpendicularly propagate upon the spherical wavefronts, said radio waves possess a wavelength twice the wavelength of the acoustic wave.

6. The apparatus according to claim 3, wherein the pulse acoustic wave source transmits a pulse of acoustic wave of 130 to 150 dB SPL.

7. The apparatus according to claim 3, wherein the radio wave source transmits a continuous wave having a frequency within the range of from 300 to 3000 MHz and a wavelength within the range of from 0.1 to 1.0 m.

8. An apparatus for the remote measurement of wind direction and speed, comprising a receiving antenna network formed of a plurality of receiving antennas laid out on the ground in the pattern of a lattice, a radio wave transmitting antenna and a pulse acoustic wave source disposed as paired near the center of each of the four sides of said receiving antenna network, said transmitting antenna and said source being positioned close to each other, a surface temperature measuring means for setting the frequency of the pulse acoustic wave transmitted by said pulse acoustic wave sources, a tone-burst signal generator for setting the cycle and pulse width of said pulse acoustic wave, a pulse acoustic wave transmission indicator adapted to measure the wind direction on the ground and issue a command for causing, among the four pulse acoustic wave sources, the windward one selectively to transmit the pulse acoustic wave, a radio wave transmitter for transmitting a continuous radio wave through said radio wave transmitting antennas toward the spherical wavefronts formed by the pulse acoustic wave transmitted by said pulse acoustic wave source vertically into the atmosphere, a wind direction and speed calculator adapted to cause the radio waves reflected by said spherical wavefronts to be received by said receiving antenna network, detect the positions of the receiving antennas in the antenna network which have received the reflected radio waves of maximum magnitude, trace the time-course change of these positions and, based on the data thus collected, calculate the height distribution of wind direction and speed, and a wind direction and speed display-record device for displaying and recording the height distribution of wind direction and speed.

9. The apparatus according to claim 8, wherein the radio waves are transmitted toward the spherical wavefronts at a wavelength such that, at the time that the waves perpendicularly propagate upon the spherical wavefronts, said radio waves possess a wavelength twice the wavelength of the acoustic wave.

10. The apparatus according to claim 8, wherein the pulse acoustic wave source transmits a pulse of acoustic wave of 130 to 150 dB SPL.

11. The apparatus according to claim 8, wherein the radio wave source transmits a continuous wave having a frequency within the range of from 300 to 3000 MHz and a wavelength within the range of from 0.1 to 1.0 m.