Wind profile with the VAD technique

The VAD (Velocity Azimuth Display) technique can be used to retrieve the vertical wind profile at the radar site with a Doppler radar. PPI scans at an elevation of about 20° cover various heights with one scan (Fig. 1).


Measurements of the Doppler velocity along a circle at constant range (= constant height) within a homogeneous wind field show a sine-function like shape (Fig. 2). The Doppler velocity has ist maximum value in the down wind direction, and ist minimum in the up wind direction. The phase angle of the minimum gives the wind direction (250° in the example). Besides the horizontal wind velocity, the Doppler velocity at elevated scans depends also on the falling velocity of the scattering particles. This portion is independent of the azimuth angle and results in an negative offset of the sine curve. The offset is shown in Fig. 2 by the dashed line. The wind velocity is the amplitude of the sine curve with respect to the offset (5 m/s in the example).

Fig.1 Estimation of the wind profile with a PPI at elevation phi. r1 to r3 are different ranges from the radar.


Fig. 2 Velocity Azimuth Display (VAD) of the Doppler velocity along a circle. Shown are data points and fitted sine curve.

VAD analysis on different ranges gives the wind profile above the radar. Wind vectors are the average value over the scaned circle. With assumptions on the falling velocity of the particles (e.g. using relations between reflectivity and terminal fall velocity) it is possible to estimate the offset. The residual offset can then be interpretated to be a result of the divergence of the wind field within the circel area. It is also possible to estimate the deformation of the wind field (see references).

References:

Browning, K.A., and R. Wexler, 1968:
The determination of kinematic properties of a wind field using Doppler radar. J. Appl. Meteor., 8, 105-113.
Lhermitte, R.M., and D.A. Atlas, 1961:
Precipitation motion by pulse Doppler radar. Proc. 9th Weather Radar Conf., Boston, Amer. Meteor. Soc., Boston, 498-503.

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