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Validation and Application of Wind Profiler Measurements of Atmospheric Turbulence

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Figure

Figure 1.1: Diagram of energy spectrum, E(k) as a function of wave number k; in theupper atmosphere, the spectrum increases at small k due to the presence of gravitywaves, whereas in the boundary layer, the spectrum decreases at small k.
Figure 1.2: Vertical proles of temperature (left) and pressure (right) in the atmo-sphere (from Doviak and Zrnic, 1984).
Figure 1.3: Schematical diagram of the Doppler Beam Swing (DBS) method. In thisgure, α and −α are zenith angles.
Table 1.1: The Walsingham radar parameters
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