Abstract
Sodar echogram is a usual means to estimate the height of temperature inversion. Our data of long-term synchronous measurements with sodar and microwave profiler in urban and rural areas showed an intricate relation between intensity of backscattering and potential temperature profiles. Qualitative relationships between echogram pattern, wind speed and temperature profiles were obtained. Distributions of temperature gradients in rural and urban measurements for summer and winter time were calculated.
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Schedule a callMore From: IOP Conference Series: Earth and Environmental Science
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