Use of 2D-video disdrometer to derive mean density–size and Ze–SR relations: Four snow cases from the light precipitation validation experiment

• Published in: Atmospheric research 2015-02, Vol.153, p.34-48
• Main Authors: Huang, Gwo-Jong, Bringi, V.N., Moisseev, Dmitri, Petersen, W.A., Bliven, L., Hudak, David
• Format: Article
• Language: English
• Subjects: Disdrometer; Radar reflectivity; Snow density; Snow rate
• ISSN: 0169-8095; 1873-2895
• DOI: 10.1016/j.atmosres.2014.07.013

The application of the 2D-video disdrometer to measure fall speed and snow size distribution and to derive liquid equivalent snow rate, mean density–size and reflectivity–snow rate power law is described. Inversion of the methodology proposed by Böhm provides the pathway to use measured fall speed, area ratio and ‘3D’ size measurement to estimate the mass of each particle. Four snow cases from the Light Precipitation Validation Experiment are analyzed with supporting data from other instruments such as the Precipitation Occurrence Sensor System (POSS), Snow Video Imager (SVI), a network of seven snow gauges and three scanning C-band radars. The radar-based snow accumulations using the 2DVD-derived Ze–SR relation are in good agreement with a network of seven snow gauges and outperform the accumulations derived from a climatological Ze–SR relation used by the Finnish Meteorological Institute (FMI). The normalized bias between radar-derived and gauge accumulation is reduced from 96% when using the fixed FMI relation to 28% when using the Ze–SR relations based on 2DVD data. The normalized standard error is also reduced significantly from 66% to 31%. For two of the days with widely different coefficients of the Ze–SR power law, the reflectivity structure showed significant differences in spatial variability. Liquid water path estimates from radiometric data also showed significant differences between the two cases. Examination of SVI particle images at the measurement site corroborated these differences in terms of unrimed versus rimed snow particles. The findings reported herein support the application of Böhm's methodology for deriving the mean density–size and Ze–SR power laws using data from 2D-video disdrometer. •Use 2DVD to measure the fall speed, area ratio and ‘3D’ size of snowflake and compute the snow size distribution (SSD).•Inverted Böhm’s equation to estimate the density-size relations. Use SSD and density-size relation to compute Ze and liquid equivalent snow rate (SR) and fit to a daily Z-SR power-law relation.•4 winter events from LPVEx are analyzed.•Apply Z-SR relation along with 3 FMI C-band radars to compute daily accumulated SR and compare them with 7 FMI snow gauges.