摘要
利用北京325m气象塔资料对1993年4月9日北京地区出现的一次特大强风过程的边界层结构(风、温、风切变及阵风特征)进行了分析。随着该次大风的过境,边界层内风场出现数个风速高值中心,高度位于200~300m,时间间隔1~3h。伴随上层风速垂直切变和阵风特性。湍流能谱的计算结果表明了大尺度涡旋对边界层湍流微结构的影响。
Using the data of the 325 m Beding Meteorological Tower, the structures of wind and temperature of a strong wind event occurred in the Beijing area on April 9, 1993 are analyzed. During the passage of the strong wind, the wind field in the boundary layer appeared several maximum regions at the 200~300 m level with time intervals of 1~3 h. Accompanying those at the upper level, there apPeared very strong wind vertical shear and wind gustness in the lower layer, whiCh also fluctuated with time. The temperature field appeared several inconsistent 'turning' with time. All these reflect the special structure in the boundary layer during the approaching of a severe weather. The result of turbulent spectra shows that during the strong wind, the contributions of vortexes on different scales to turbulent energy at different heights are not the same, which reflects the influence of large scale vortex on the fine structure of turbulence in the atmospheric boundary layer.
出处
《大气科学》
CSCD
北大核心
1996年第2期223-228,共6页
Chinese Journal of Atmospheric Sciences
基金
国家自然科学青年基金
国家博士后基金
关键词
强风
边界层结构
大风
湍流能谱
北京地区
strong wind structure of atmospheric boundary layer turbulent spectra