FIELD: physics.
SUBSTANCE: atmosphere is probed with two pulsed laser beams propagating with a small angular distance between them of up to 10 degrees and signals from scattering volumes of aerosol non-uniformities are then picked up. The atmosphere is irradiated with laser pulses with duration of  , defined by minimum distance dmin between scattering volumes in the atmosphere and speed of light C. The number of scattering volumes n > 2 is selected based on the required angular accuracy Δφ for determining wind direction. Minimum values
, defined by minimum distance dmin between scattering volumes in the atmosphere and speed of light C. The number of scattering volumes n > 2 is selected based on the required angular accuracy Δφ for determining wind direction. Minimum values  of mutual-structure functions S1,i(τ)=([U1(t)-Ui(t+τ)]2) between a signal U1(t) from scattering volume 1 of the first beam and signal Ui(t), i=2…n from scattering volumes 2…i…n of the second beam are determined. The wind direction is the direction between scattering volume 1 and the scattering volume with the least minimum value
 of mutual-structure functions S1,i(τ)=([U1(t)-Ui(t+τ)]2) between a signal U1(t) from scattering volume 1 of the first beam and signal Ui(t), i=2…n from scattering volumes 2…i…n of the second beam are determined. The wind direction is the direction between scattering volume 1 and the scattering volume with the least minimum value  of the mutual-structure function. The value and sign of the wind speed is determined from the time position of the minimum of the mutual-structure function of signals for these scattering volumes and from the distance between these volumes.
 of the mutual-structure function. The value and sign of the wind speed is determined from the time position of the minimum of the mutual-structure function of signals for these scattering volumes and from the distance between these volumes.
EFFECT: higher accuracy of real-time remote determination of wind speed and direction.
2 dwg, 2 tbl
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| 0 | 
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| RADAR TOMOGRAPHIC SYSTEM FOR MEASUREMENT OF WIND FLOW PARAMETERS | 2023 | 
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| METHOD AND LIDAR SYSTEM FOR MEASURING ATMOSPHERIC TURBULENCE ON-BOARD AIRCRAFT, AS WELL AS IN AIRPORTS AND ON WIND POWER PLANTS | 2006 | 
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| METHOD OF DETERMINING MOST PROBABLE VALUES OF BEARINGS OF RADIO-FREQUENCY SOURCES AT ONE FREQUENCY | 2012 | 
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Authors
Dates
2010-11-20—Published
2009-06-04—Filed