首页 | 本学科首页   官方微博 | 高级检索  
     检索      

华北北部半干旱地区夏季大气边界层特征的实验研究
引用本文:李倩惠,张宏升,鞠婷婷,肖凯涛.华北北部半干旱地区夏季大气边界层特征的实验研究[J].北京大学学报(自然科学版),2020,56(2):215-222.
作者姓名:李倩惠  张宏升  鞠婷婷  肖凯涛
作者单位:1. 北京大学物理学院大气与海洋科学系, 气候与海?气实验室, 北京 100871 2. 军事科学院防化研究院, 北京 100091
基金项目:国家自然科学基金(41544216)和国家重点研发计划(2017YFC0209600, 2016YFC0203300)资助
摘    要:2016年7月3—16日在内蒙古自治区科尔沁地区大气科学与大气环境综合实验站开展科尔沁半干旱下垫面大气边界层野外综合观测试验, 利用 GPS大气边界层精细探空资料, 分析华北北部半干旱地区晴天、阴天和雨天等不同天气条件下的大气边界层结构。采取不同的方法和判据对比确定大气边界层高度, 统计实验期间低空急流特征, 并对近地面湍流特征及地表能量收支状况进行初步的探讨。结果表明: 晴天, 白天的大气边界层平均高度约为1790 m, 夜间约为250 m; 阴天和雨天, 白天的大气边界层平均高度约为980 m, 夜间约为430 m。夜间, 近地面层湍流动能与边界层高度有较强的相关性。低空急流多发生在午夜, 平均高度约为390 m, 强度与高度正相关。

关 键 词:大气边界层高度  低空急流  地表能量收支  半干旱地区  
收稿时间:2019-03-27

Experimental Research on the Characteristics of the Atmospheric Boundary Layer in the Semi-arid North China
LI Qianhui,ZHANG Hongsheng,JU Tingting,XIAO Kaitao.Experimental Research on the Characteristics of the Atmospheric Boundary Layer in the Semi-arid North China[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2020,56(2):215-222.
Authors:LI Qianhui  ZHANG Hongsheng  JU Tingting  XIAO Kaitao
Institution:1. Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871

2. Research Institution of Chemical Defense, Academy of Military Sciences, Beijing 100091

Abstract:A comprehensive experiment on semi-arid underlying surface was carried out at the comprehensive experimental station of atmospheric science and atmospheric environment in Horqin, Inner Mongolia during July 3th to 16th in 2016. Using high-precision GPS sounding data of the atmospheric boundary layer (ABL), the structure of the ABL in the semi-arid North China under different weather conditions (sunny, cloudy and rainy) was analyzed. The atmospheric boundary layer height (ABLH) was determined by different methods and criteria. In addition, the characteristics of low-level jets (LLJs), surface turbulent flux and surface energy budget were discussed. The results indicate that the average height of the ABL is 1790 m during the day while it is 250 m at night when sunny. In the cloudy day, the average ABLH is 980 m in daytime and 430 m at night. The turbulent kinetic energy in the surface layer shows a strong correlation with ABLH at night. LLJs mostly occur at midnight, with an average altitude of approximately 390 m, and there is a positive correlation between the intensity and the altitude of LLJs.
Keywords:atmospheric boundary layer height  low-level jet  surface energy budget  semi-arid area  
本文献已被 CNKI 等数据库收录!
点击此处可从《北京大学学报(自然科学版)》浏览原始摘要信息
点击此处可从《北京大学学报(自然科学版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号