Field investigation of 3D snow settling dynamics under weak atmospheric turbulence

TL;DR

This study provides a detailed field analysis of 3D snow particle settling under weak turbulence, revealing how particle shape and orientation influence velocity and trajectory, improving snow accumulation models.

Contribution

It introduces a comprehensive 3D field measurement approach for snow settling, highlighting discrepancies in aerodynamic predictions for non-spherical particles and analyzing their complex trajectories.

Findings

Graupels' terminal velocity matches models, but dendrites show higher drag.

Aggregates and dendrites exhibit pronounced meandering trajectories.

Meandering frequencies relate to particle shape and atmospheric turbulence.

Abstract

Research on settling dynamics of snow particles, considering their complex morphologies and real atmospheric conditions, remains scarce despite extensive simulations and laboratory studies. Our study bridges the gap through a comprehensive field investigation into the three-dimensional (3D) snow settling dynamics under weak atmospheric turbulence, enabled by a 3D particle tracking velocimetry (PTV) system to record > a million trajectories, coupled with a snow particle analyzer for simultaneous aerodynamic property characterization of four distinct snow types (aggregates, graupels, dendrites, needles). Our findings indicate that while the terminal velocity predicted by the aerodynamic model aligns well with PTV-measured settling velocity for graupels, significant discrepancies arise for non-spherical particles, particularly dendrites, which exhibit higher drag coefficients than predicted. Qualitative observations of 3D settling trajectories highlight pronounced meandering in aggregates and dendrites, in contrast to the subtler meandering observed in needles and graupels, attributable to their smaller frontal areas. This meandering in aggregates and dendrites occurs at lower frequencies compared to that of graupels. Further quantification of trajectory acceleration and curvature suggests that the meandering frequencies in aggregates and dendrites are smaller than that of morphology-induced vortex shedding of disks, likely due to their rotational inertia, and those of graupels align with the small-scale atmospheric turbulence. Moreover, our analysis of vertical acceleration along trajectories elucidates that the orientation changes in dendrites and aggregates enhance their settling velocity. Such insights into settling dynamics refine models of snow settling velocity under weak atmospheric turbulence, with broader implications for more accurately predicting ground snow accumulation.