Raindrop fall velocities from an optical array probe and 2-D video disdrometer

Abstract

We report on fall speed measurements of raindrops in light-to-heavy rain events from two climatically different regimes (Greeley, Colorado, and Huntsville, Alabama) using the high-resolution (50 μm) Meteorological Particle Spectrometer (MPS) and a third-generation (170 μm resolution) 2-D video disdrometer (2DVD). To mitigate wind effects, especially for the small drops, both instruments were installed within a 2=3-scale Double Fence Intercomparison Reference (DFIR) enclosure. Two cases involved light-tomoderate wind speeds/gusts while the third case was a tornadic supercell and several squall lines that passed over the site with high wind speeds/gusts. As a proxy for turbulent intensity, maximum wind speeds from 10m height at the instrumented site recorded every 3 s were differenced with the 5 min average wind speeds and then squared. The fall speeds vs. size from 0.1 to 2 and > 0:7mm were derived from the MPS and the 2DVD, respectively. Consistency of fall speeds from the two instruments in the overlap region (0.7-2 mm) gave confidence in the data quality and processing methodologies. Our results indicate that under low turbulence, the mean fall speeds agree well with fits to the terminal velocity measured in the laboratory by Gunn and Kinzer from 100 μm up to precipitation sizes. The histograms of fall speeds for 0.5, 0.7, 1 and 1.5mm sizes were examined in detail under the same conditions. The histogram shapes for the 1 and 1.5mm sizes were symmetric and in good agreement between the two instruments with no evidence of skewness or of sub- or super-terminal fall speeds. The histograms of the smaller 0.5 and 0.7mm drops from MPS, while generally symmetric, showed that occasional occurrences of suband super-terminal fall speeds could not be ruled out. In the supercell case, the very strong gusts and inferred high turbulence intensity caused a significant broadening of the fall speed distributions with negative skewness (for drops of 1.3, 2 and 3 mm). The mean fall speeds were also found to decrease nearly linearly with increasing turbulent intensity attaining values about 25-30% less than the terminal velocity of Gunn-Kinzer, i.e., sub-terminal fall speeds.