Abstract I have measured time series of the turbulent fluctuations in longitudinal (u) and vertical (w) velocity and in temperature (t) and humidity (q) with fast-responding sensors in the near-neutrally stable surface layer over a snow-covered field. The series yielded individual spectra, u-w, w-t, w-q, and t-q cospectra and phase and coherence spectra for nondimensional frequencies (fz/U) from roughly 0.001 to 10. This is, thus, one of the most extensive spectral sets over collected over a snow-covered surface. With the exception of the u-w cospectra, all of the spectra and cospectra displayed the expected dependence on frequency in an inertial or inertial-convective subrange. All, however, contained significantly move energy at low frequency than the Kansas neutral-stability spectra and cospectra. This excess low-frequency energy and the erratic behavior of the u-w cospectra imply that the forested bills bordering the site on two sides were producing disturbances in the flow field at scales roughly equ...
CITATION STYLE
Andreas, E. L. (1987). Spectral Measurements in a Disturbed Boundary Layer over Snow. Journal of the Atmospheric Sciences, 44(15), 1912–1939. https://doi.org/10.1175/1520-0469(1987)044<1912:smiadb>2.0.co;2
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