PICTURE

Doppler spectra of migrating insects

1998-02-25 Matti Leskinen
The figure shows calculated Doppler-spectra in clear air echoes about 5 kilometers from Doppler weather radar in Helsinki on October 9, 1991. The direction of the measurement is to the Gulf of Finland (SSE). The weather was foggy in Southern Finland and temperatures were about +10°C at maximum. On the other side of the Gulf of Finland in Estonia the sky was clear and maximum temperatures were over +20°C.

The Doppler-spectrum indicates how the echo power is distributed according to the Doppler-shift frequency. The Doppler-shift frequency is directly related to the radial velocity of the scatterer. A pulsed Doppler radar uses phase change of the echo between pulses to calculate the Doppler shift frequency and consequently only velocities that correspond to radial displacements smaller than a fourth of wavelength in pulse repetition period are unaliased. In the picture the unaliased velocity intervall is ±5 m/s.

The ranges of the 10 spectra displayed are shown in kilometers on the right hand side of the picture. The velocity range of the spectra goes from 5 m/s towards the radar at the left end and 5 m/s away from the radar at the right end of the points
The relatively thin peaks in the spectra are caused by relatively large insects. According to Kauri Mikkola (Finnish Museum of Natural History) the moth species involved was probably Agriopis aurantiaria. The measurement lasted 0.34 seconds and the differences in the speeds are mostly explained by the individual differences in the flight directions and speeds of the insects. However, the calculated mean motion using many pulse volumes is near the wind speed and direction.


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Matti Leskinen
Department of Meteorology