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Measurements Of Blowing Snow, Part I: Particle Shape, Size Distribution, Velocity, And Number Flux At Churchill, Manitoba, Canada

机译:吹雪的测量,第一部分:加拿大曼尼托巴丘吉尔市的颗粒形状,尺寸分布,速度和数通量

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Blowing snow is a frequent and significant winter weather event, and there is currently a need for more observations and measurements of blowing snow, especially in arctic and subarctic environments. This is the first paper in a two part series studying blowing snow in Churchill, Manitoba, and Franklin Bay, NWT. In this part, the development and use of a camera system to measure the shape, size and velocity of blowing snow particles is described. This system was used, along with standard meteorological instruments and optical particle counters, during field campaigns at Churchill, MB, which took place in March, 2005 and December, 2006. Measurements of blowing snow particle shape demonstrate that blowing snow particles are generally non-spherical, with an average ratio of the longest particle profile length to the perpendicular width of 1.41. Measurement of particle velocity with the camera system is shown to be inaccurate. However, measurements of particle number correlate well (r~2=0.85) with simultaneous measurements made with a particle counter at the same height as the camera. The particle size distributions generally follow a Gamma distribution, with an average shape parameter of α=1.9. The shape parameter, α, shows no trend with height. The blowing snow particle number density decreases with height as approximately N ∝ z~(-1.4). The blowing snow particle number densities, interpolated to a height of 0.1 m, are in the range of 1.4×10~5 < N < 4.7×10~7 m~(-3). Particle number densities are shown to generally increase over a limited range of wind speeds, corresponding to 10-m wind speeds in the range of 13 < U_(10) < 17 m s~(-1). Over this range of wind speeds, the average particle size at a given height does not change significantly with wind speed. However, at a lower wind speed of U_(10) ≈ 9 m s~(-1), the average particle size is generally smaller. Particle sizes generally decrease with height between 0.06 and 1 m. Above 0.2 m, the average particle diameters found in this study (120 μm
机译:吹雪是冬季经常发生的重大天气事件,目前需要对吹雪进行更多的观测和测量,尤其是在北极和亚北极环境中。这是一个分为两部分的系列文章的第一篇,该系列文章研究了曼尼托巴省丘吉尔和西北地区富兰克林湾的吹雪。在这一部分中,描述了用于测量吹雪粒子的形状,大小和速度的相机系统的开发和使用。在2005年3月和2006年12月在MB丘吉尔举行的野外运动中,使用了该系统以及标准的气象仪器和光学粒子计数器。吹雪粒子形状的测量结果表明,吹雪粒子通常不是球形,最长颗粒轮廓长度与垂直宽度的平均比为1.41。用相机系统测量粒子速度是不准确的。然而,粒子数的测量与使用与照相机相同高度的粒子计数器进行的同时测量具有很好的相关性(r〜2 = 0.85)。粒度分布通常遵循Gamma分布,平均形状参数为α= 1.9。形状参数α没有显示出高度的趋势。吹雪颗粒数密度随高度降低而降低,大约为N ∝ z〜(-1.4)。内插到0.1 m高度的吹雪颗粒数密度在1.4×10〜5

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