Elucidation of spatiotemporal structures from high-resolution blowing-snow observations

Systematic observations were conducted to investigate the spatiotemporal structures of blowing snow. Along a line perpendicular to the dominant wind direction on the lee side of a flat field, 15 snow particle counters (SPCs) and ultrasonic anemometers (USAs) were placed 1.5 m apart. Data were record...

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Published inThe cryosphere Vol. 18; no. 10; pp. 4775 - 4786
Main Authors Nishimura, Kouichi, Nemoto, Masaki, Ito, Yoichi, Omiya, Satoru, Shimoyama, Kou, Niiya, Hirofumi
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 22.10.2024
Copernicus Publications
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Summary:Systematic observations were conducted to investigate the spatiotemporal structures of blowing snow. Along a line perpendicular to the dominant wind direction on the lee side of a flat field, 15 snow particle counters (SPCs) and ultrasonic anemometers (USAs) were placed 1.5 m apart. Data were recorded at high frequencies of 100 kHz for SPCs and 1 kHz for USAs. The horizontal mass flux distributions, representing the spatiotemporal variability of blowing snow, exhibited non-uniformity in both time and space and manifested periodic changes akin to snow waves. Additionally, the presence of “snow snakes”, meandering near the snow surface, was observed. Quadrant analysis revealed predominant snow fluxes in quadrants Q1 (u′>0, w′>0) and Q4 (u′>0, w′<0). However, a more detailed parametric curve analysis indicated the existence of ejection events in Q2 (u′<0, w′>0) before snow waves and in front of snow snakes, shifting to Q1 and Q4 afterward, implying the consideration of both top-down and bottom-up mechanisms for burst sweep events.
ISSN:1994-0424
1994-0416
1994-0424
1994-0416
DOI:10.5194/tc-18-4775-2024