Characteristics of energy dissipation rate and effect of humidity on turbulence echo power revealed by MU radar-RASS Measurements

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Scientific paper

We carried out an MU radar-RASS campaign during August 2-6, 1995, and collected both radar echoes and virtual temperatures with good time resolution. We first investigated the accuracy of the Brunt-Väisälä frequency squared from the RASS temperature profiles, comparing them with radiosonde results launched from the radar site. We then evaluated the turbulence energy dissipation rate (/ɛ) by two radar methods: the Doppler spectral width and the radar echo power. Meteorological conditions were very calm throughout the campaign, which is ideal for deriving /ɛ by the spectral width method. Under calm conditions, the variation of /ɛ from spectral width is mainly influenced by the Doppler spectral width and is less dependent on the Brunt-Väisälä frequency. On the other hand, /ɛ from echo power is mainly determined by the echo power intensity. Though /ɛ values from both methods are roughly on the same order, their characteristics differ significantly. /ɛ with spectral width did not show large variations with time and height, while /ɛ with echo power showed significant fluctuations. We suspect that /ɛ from echo power is inaccurate because the refractive-index gradient in the calculation of /ɛ is mainly controlled by the humidity gradient in moist regions.

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