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作 者:张镭[1] 王世红[1] 任健美[1] 张武[1] 陈长和[1]
出 处:《兰州大学学报(自然科学版)》1994年第4期152-156,共5页Journal of Lanzhou University(Natural Sciences)
基 金:甘肃省环境科学基金
摘 要:本文利用若干次低山丘陵地区的Gill双向风标风速仪资料,按Hay-Pasquill方法计算了此类地区的大气扩散参数,讨论了其特征及其与P-G扩散参数的差别.发现低山丘陵地区的各级别扩散曲线间截距差比P-G曲线的小很多;曲线的斜率也比P-G曲线的小.σy在稳定和中性情况下,比P-G曲线高2-3级;在不稳定条件下,高1-2级,σz在稳定和中性情况下,高1.5级;不稳定情况下,平均高1级。Based on a series of data collected by Gill bivance anemometer the atmospheric diffusion parameters of hilly areas are estimated by the Hay-Pasquill method, and the difference between the estimation and the P-G diffusion curves is also discussed. It shows that the nodal increment difference of the diffusion curves in the areas is much smaller in comparison with that of P-G diffusion curves, and the slope of the diffusion curves is again smaller than that of the P-G diffusion curves. In a neutral and stable situation the σy curves are 2 ̄3 classes higher than the P-G curves while 1 ̄2 classes higher in an unstable situation. The σz.curves are 1. 5 classes higher in a stable and neutral situation and the average increase is one class in an unstable situation.
分 类 号:X16[环境科学与工程—环境科学]
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