摘要
首先探讨了常规气象资料计算大气边界层厚度的方法,然后利用全国125个无线电探空站的观测资料,计算了我国早晨与傍晚时的大气边界层厚度h,并分析了h的地区分布与季节变化特征。结果表明,华南地区边界层厚度年平均值最大(h>500m);陕甘宁地区最小(h=318m);多数地区的h值在冬季最小而夏季或春季最大。
This paper discussed firstly the method of calculating atmospheric boundary-layer thickness (h) based on conventional atmosphere data.Then,authors figured out h values over China in the morning and the evening and analyzed the characters of their regional distributions and seasonal variations utilizing observed data from 125 radiosondage stations in China.The results indicated that the annual mean thickness value of over 500m in South China reached the peak value,that of 318m in Shanxi,Gansu,Ningxia region was the lowets,and the h value of most regions in China changed from minimum in winter to maximum in summer or spring.
出处
《油气田环境保护》
CAS
1998年第3期31-34,共4页
Environmental Protection of Oil & Gas Fields
关键词
中国
大气层
厚度
污染物
大气污染
atmospheric boundary-layer, thickness, change, distribution, calculation