Thermal structure of the atmospheric boundary layer over the South African Mpumalanga Highveld

被引:3
作者
Becker, S [1 ]
机构
[1] Univ Wisconsin, Dept Geog & Urban Planning, Oshkosh, WI 54901 USA
关键词
thermal atmospheric stability; atmospheric boundary layer; vertical potential air-temperature lapse rate;
D O I
10.3354/cr029129
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study deals with the parametrisation of the vertical thermal structure of the atmospheric boundary layer up to 100 in above ground level over the industrial Mpumalanga Highveld in South Africa. Potential air temperatures were calculated by similarity theory based algorithms. The results were unsatisfactory for stable and unstable conditions in comparison to the measured data of a 96 m tower. A higher accuracy was achieved with algorithms constructed by subjecting the measured data to multiple regression analysis. Potential air temperatures at various levels up to 96 m above ground level were calculated with average errors of 0.82 degrees C for stable conditions, 0.63 degrees C for unstable early-morning and late-afternoon conditions and 0.37 degrees C for unstable daytime conditions. The accuracy was sufficient to assess the thermal atmospheric stability of the boundary layer up to 100 m above ground level.
引用
收藏
页码:129 / 137
页数:9
相关论文
共 9 条
[1]  
ESKOM, 1994, STAT YB 1993
[2]  
Held G., 1996, AIR POLLUTION ITS IM
[3]  
JACOBSEN MZ, 1999, FUNDAMENTALS ATMOSPH
[4]  
LOUIS JF, 1979, BOUND-LAY METEOROL, V17, P87
[5]  
Monin A. S., 1954, Trudy geofiz. inst. AN SSSR, V24, P163, DOI DOI 10.2514/6.2012-537
[6]  
Oke T. R., 1987, BOUNDARY LAYER CLIMA, V2nd
[7]  
PICHLER H, 1997, DYNAMIK ATMOSPHARE
[8]  
Preston-Whyte R., 1993, ATMOSPHERE WEATHER S
[9]  
Roedel W., 2000, PHYSIK UNSERER UMWEL