Vertical Velocity Variance in the Mixed Layer from Radar Wind Profilers

• Published in: Journal of hydrologic engineering 2003-11, Vol.8 (6), p.301-307
• Main Authors: Eng, Ken, Coulter, Richard L, Brutsaert, Wilfried
• Format: Article
• Language: English
• Subjects: TECHNICAL PAPERS
• ISSN: 1084-0699; 1943-5584
• DOI: 10.1061/(ASCE)1084-0699(2003)8:6(301)

Vertical velocity variance data were derived from remotely sensed mixed layer turbulence measurements at the Atmospheric Boundary Layer Experiments (ABLE) facility in Butler County, Kansas. These measurements and associated data were provided by a collection of instruments that included two 915 MHz wind profilers, two radio acoustic sounding systems, and two eddy correlation devices. The data from these devices were available through the Atmospheric Boundary Layer Experiment (ABLE) database operated by Argonne National Laboratory. A signal processing procedure outlined by Angevine et al. was adapted and further built upon to derive vertical velocity variance, w′2¯, from 915 MHz wind profiler measurements in the mixed layer. The proposed procedure consisted of the application of a height-dependent signal-to-noise ratio (SNR) filter, removal of outliers plus and minus two standard deviations about the mean on the spectral width squared, and removal of the effects of beam broadening and vertical shearing of horizontal winds. The scatter associated with w′2¯ was mainly affected by the choice of SNR filter cutoff values. Several different sets of cutoff values were considered, and the optimal one was selected which reduced the overall scatter on w′2¯ and yet retained a sufficient number of data points to average. A similarity relationship of w′2¯ versus height was established for the mixed layer on the basis of the available data. A strong link between the SNR and growth/decay phases of turbulence was identified. Thus, the mid to late afternoon hours, when strong surface heating occurred, were observed to produce the highest quality signals.