Snow Studies. Part II: Average Relationship between Mass of Snowflakes and Their Terminal Fall Velocity

@article{Szyrmer2010SnowSP,
  title={Snow Studies. Part II: Average Relationship between Mass of Snowflakes and Their Terminal Fall Velocity},
  author={Wanda Szyrmer and Isztar Zawadzki},
  journal={Journal of the Atmospheric Sciences},
  year={2010},
  volume={67},
  pages={3319-3335}
}
Abstract This study uses a dataset of low-density snow aggregates measurements collected by a ground-based optical disdrometer that provides particle size and terminal fall speed for each size interval from which the velocity–size and area ratio–size relationships can be derived. From these relationships and relations between the Best and Reynolds numbers proposed in the literature, the mass power-law coefficients are obtained. Then, an approximate average relation between the coefficients in… 

Ensemble mean density and its connection to other microphysical properties of falling snow as observed in Southern Finland

Abstract. In this study measurements collected during winters 2013/2014 and 2014/2015 at the University of Helsinki measurement station in Hyytiala are used to investigate connections between

Mass of different snow crystal shapes derived from fall speed measurements

Abstract. Meteorological forecast and climate models require good knowledge of the microphysical properties of hydrometeors and the atmospheric snow and ice crystals in clouds. For instance, their

Microphysical Properties of Snow and Their Link to Ze–S Relations during BAECC 2014

AbstractThis study uses snow events from the Biogenic Aerosols–Effects on Clouds and Climate (BAECC) 2014 campaign to investigate the connection between properties of snow and radar observations. The

Snow Studies. Part III: Theoretical Derivations for the Ensemble Retrieval of Snow Microphysics from Dual-Wavelength Vertically Pointing Radars

AbstractAs a first step toward retrieval of snow microphysics from two vertically pointing radars operating at X band and W band, a theoretical model of snow microphysics is formulated in which the

Polarimetric Radar Relations for Quantification of Snow Based on Disdrometer Data

AbstractAccurate measurements of snow amounts by radar are very difficult to achieve. The inherent uncertainty in radar snow estimates that are based on the radar reflectivity factor Z is caused by

Assessing the Effect of Riming on Snow Microphysics: The First Observational Study in East China

Through the collision and freezing of supercooled droplets on the surface of snow particles, riming can change the density, fall velocity and aspect ratio of snow particles. Riming plays an important

Dual-wavelength radar technique development for snow rate estimation: a case study from GCPEx

Abstract. quantitative precipitation estimation (QPE) of snowfall has generally been expressed in power-law form between equivalent radar reflectivity factor (Ze) and liquid equivalent snow rate

Snow Studies. Part IV: Ensemble Retrieval of Snow Microphysics from Dual-Wavelength Vertically Pointing Radars

AbstractBased on the theory developed in Part III, this paper introduces a new method to retrieve snow microphysics from ground-based collocated X- and W-band vertically pointing Doppler radars. To

Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea

Snow particle size distribution (PSD) information is important in understanding the microphysics and quantitative precipitation estimation over complex terrain. Measurement and interpretation of the
...

References

SHOWING 1-10 OF 53 REFERENCES

Assessing Snowfall Rates from X-Band Radar Reflectivity Measurements

Abstract Realistic aggregate snowflake models and experimental snowflake size distribution parameters are used to derive X-band power-law relations between the equivalent radar reflectivity factor Ze

Refinements to Ice Particle Mass Dimensional and Terminal Velocity Relationships for Ice Clouds. Part I: Temperature Dependence

Abstract This two-part study attempts to find appropriate mass dimension and terminal velocity relationships that, when considered together with particle size distributions (PSD), agree with

A Statistical and Physical Description of Hydrometeor Distributions in Colorado Snowstorms Using a Video Disdrometer

Abstract Winter-storm hydrometeor distributions along the Front Range in eastern Colorado are studied with a ground-based two-dimensional video disdrometer. The instrument provides shape, size, and

Snow Studies. Part I: A Study of Natural Variability of Snow Terminal Velocity

Abstract The variability and the uncertainties in snowfall velocity measurements are addressed in this study. The authors consider (i) the instrumental uncertainty in the fall velocity measurement,

Mass-Dimensional Relationships for Ice Particles and the Influence of Riming on Snowfall Rates

Abstract The masses, dimensions, and habits of over 2800 natural ice particles precipitating from orographic winter storms in the central Sierra Nevada were obtained using photomicrographs. Ice

A Methodology to Derive Radar Reflectivity–Liquid Equivalent Snow Rate Relations Using C-Band Radar and a 2D Video Disdrometer

Abstract The objective of this work is to derive equivalent radar reflectivity factor–liquid equivalent snow rate (Ze–SR) power-law relations for snowfall using the C-band King City operational

A general approach for deriving the properties of cirrus and stratiform ice cloud particles

A new approach is described for calculating the mass (m) and terminal velocity (Vt) of ice particles from airborne and balloon-borne imaging probe data as well as its applications for remote sensing

The terminal velocity of snowflakes

Measurements of the terminal velocity of aggregate snowflakes at the ground indicate that the velocity is approximately proportional to the one-tenth power of the mass. The constant of

Determination of a Z-R Relationship for Snowfall Using a Radar and High Sensitivity Snow Gauges

Abstract A best-fit power-law relationship (Z = 427 R1.09) between 1-minute integrated averages of snowfall rate (R) and radar reflectivity factor (Z) was determined on the basis of observations made

Aggregate Terminal Velocity/Temperature Relations

Abstract Terminal velocities of snow aggregates in storms along the Front Range in eastern Colorado are examined with a ground-based two-dimensional video disdrometer. Power-law relationships for
...