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 snow PSDs is a topic of active research. This study investigates snow PSDs during 3 year of observati...

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Main Authors: Tiantian Yu, V. Chandrasekar, Hui Xiao, Shashank S. Joshil
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/10/1093
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author Tiantian Yu
V. Chandrasekar
Hui Xiao
Shashank S. Joshil
author_facet Tiantian Yu
V. Chandrasekar
Hui Xiao
Shashank S. Joshil
author_sort Tiantian Yu
collection DOAJ
description Snow particle size distribution (PSD) information is important in understanding the microphysics and quantitative precipitation estimation over complex terrain. Measurement and interpretation of the snow PSDs is a topic of active research. This study investigates snow PSDs during 3 year of observations from Parsivel<sup>2</sup> disdrometers and precipitation imaging packages (PIP) at five different sites in the PyeongChang region of South Korea. Variabilities in the values of the density of snow (<inline-formula><math display="inline"><semantics><mi>ρ</mi></semantics></math></inline-formula>), snowfall rate (<inline-formula><math display="inline"><semantics><mi>S</mi></semantics></math></inline-formula>), and ice water content (<inline-formula><math display="inline"><semantics><mrow><mi>I</mi><mi>W</mi><mi>C</mi></mrow></semantics></math></inline-formula>) are studied. To further understand the characteristics of snow PSD at different density and snowfall rate, the snow particle size distribution measurements are divided into six classes based on the density values of snowfall and five classes based on snowfall rates. The mean shape factors (<inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula>, <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula>, and <inline-formula><math display="inline"><semantics><mi>μ</mi></semantics></math></inline-formula>) of normalized gamma distribution are also derived based on different density and snowfall rate classes. The <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> decreases and <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula> and <i>μ</i> increase as the density increases. The <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula> increase and <i>μ</i> decreases with the increase of snowfall rate. The power-law relationship between <inline-formula><math display="inline"><semantics><mi>ρ</mi></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> is obtained and the relationship between <inline-formula><math display="inline"><semantics><mi>S</mi></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><mi>I</mi><mi>W</mi><mi>C</mi></mrow></semantics></math></inline-formula> is also derived.
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spelling doaj.art-7c49cdc399884872a0c6a4b691d671b32023-11-20T16:56:03ZengMDPI AGAtmosphere2073-44332020-10-011110109310.3390/atmos11101093Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South KoreaTiantian Yu0V. Chandrasekar1Hui Xiao2Shashank S. Joshil3Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaColorado State University, Fort Collins, CO 80523, USAInstitute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaColorado State University, Fort Collins, CO 80523, USASnow particle size distribution (PSD) information is important in understanding the microphysics and quantitative precipitation estimation over complex terrain. Measurement and interpretation of the snow PSDs is a topic of active research. This study investigates snow PSDs during 3 year of observations from Parsivel<sup>2</sup> disdrometers and precipitation imaging packages (PIP) at five different sites in the PyeongChang region of South Korea. Variabilities in the values of the density of snow (<inline-formula><math display="inline"><semantics><mi>ρ</mi></semantics></math></inline-formula>), snowfall rate (<inline-formula><math display="inline"><semantics><mi>S</mi></semantics></math></inline-formula>), and ice water content (<inline-formula><math display="inline"><semantics><mrow><mi>I</mi><mi>W</mi><mi>C</mi></mrow></semantics></math></inline-formula>) are studied. To further understand the characteristics of snow PSD at different density and snowfall rate, the snow particle size distribution measurements are divided into six classes based on the density values of snowfall and five classes based on snowfall rates. The mean shape factors (<inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula>, <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula>, and <inline-formula><math display="inline"><semantics><mi>μ</mi></semantics></math></inline-formula>) of normalized gamma distribution are also derived based on different density and snowfall rate classes. The <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> decreases and <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula> and <i>μ</i> increase as the density increases. The <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><mi>l</mi><mi>o</mi><msub><mi>g</mi><mrow><mn>10</mn></mrow></msub><msub><mi>N</mi><mi>w</mi></msub></mrow></semantics></math></inline-formula> increase and <i>μ</i> decreases with the increase of snowfall rate. The power-law relationship between <inline-formula><math display="inline"><semantics><mi>ρ</mi></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><msub><mi>D</mi><mi>m</mi></msub></mrow></semantics></math></inline-formula> is obtained and the relationship between <inline-formula><math display="inline"><semantics><mi>S</mi></semantics></math></inline-formula> and <inline-formula><math display="inline"><semantics><mrow><mi>I</mi><mi>W</mi><mi>C</mi></mrow></semantics></math></inline-formula> is also derived.https://www.mdpi.com/2073-4433/11/10/1093snow PSDdensitysnowfall ratepower-law relationship
spellingShingle Tiantian Yu
V. Chandrasekar
Hui Xiao
Shashank S. Joshil
Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
Atmosphere
snow PSD
density
snowfall rate
power-law relationship
title Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
title_full Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
title_fullStr Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
title_full_unstemmed Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
title_short Characteristics of Snow Particle Size Distribution in the PyeongChang Region of South Korea
title_sort characteristics of snow particle size distribution in the pyeongchang region of south korea
topic snow PSD
density
snowfall rate
power-law relationship
url https://www.mdpi.com/2073-4433/11/10/1093
work_keys_str_mv AT tiantianyu characteristicsofsnowparticlesizedistributioninthepyeongchangregionofsouthkorea
AT vchandrasekar characteristicsofsnowparticlesizedistributioninthepyeongchangregionofsouthkorea
AT huixiao characteristicsofsnowparticlesizedistributioninthepyeongchangregionofsouthkorea
AT shashanksjoshil characteristicsofsnowparticlesizedistributioninthepyeongchangregionofsouthkorea