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首页> 外文期刊>ournal of the Meteorological Society of Japan >Water-Insoluble Particles in Spring Snow at Mt. Tateyama, Japan: Characteristics of the Shape Factors and Size Distribution in Relation with Their Origin and Transportation
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Water-Insoluble Particles in Spring Snow at Mt. Tateyama, Japan: Characteristics of the Shape Factors and Size Distribution in Relation with Their Origin and Transportation

机译:山顶春雪中的水不溶性颗粒日本立山市:形状因素和尺寸分布的特征及其起源和运输

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The number-size distribution and shape factors of water-insoluble particles (WIP) in four dirty snow layers in the spring of 2001 at Mt. Tateyama, Japan, were analyzed using scanning electron microscopy, and using optical microscopy with a digital camera. Results show that the median aspect ratio (ratio of the longest dimension b to the orthogonal width a; b/a) of the WIP varied within 1.22-1.31. Only a few particles with an aspect ratio of more than 2.5 were observed. The median circularity factor (4πS/l2; S is projection area, and l is periphery length) varied from 0.83-0.97.Combined with backward air trajectories, visibility reducing surface weather reports, additional results of rain containing Saharan dust and dry deposition samples, the number and shape factor distributions versus particle size were characterized as (1) narrower distributions of number-size and shape factors for the Saharan dust, and (2) bi-modal number-size distribution for dry deposited dust. Results suggest that the proportions of nearly spherical (higher circularity nearly 1) and less elongated (lower aspect ratio close to 1) particles were higher in the sample that had been transported a longer distance from the dust source areas.
机译:2001年春季山上4个积雪层中水不溶性颗粒(WIP)的数量大小分布和形状因子。使用扫描电子显微镜和数码相机的光学显微镜对日本馆山市进行了分析。结果表明,WIP的中位纵横比(最长尺寸b与正交宽度a的比值; b / a)在1.22-1.31之间变化。仅观察到一些长径比大于2.5的颗粒。中值圆形度因子(4πS/ l2; S是投影面积,l是外围长度)在0.83-0.97之间变化。结合后向空气轨迹,能见度降低了地面天气报告,另外的雨水包含撒哈拉粉尘和干燥沉积样品,数量和形状因子分布与粒径的关系表征为(1)撒哈拉粉尘的数量和形状因子的分布较窄,(2)干沉积粉尘的双峰数量分布。结果表明,从尘埃源区域运输了较长距离的样品中,接近球形(较高的圆形度接近1)和伸长率较小(较低的纵横比接近1)的颗粒比例更高。

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