摘要
根据在凤凰山机场和双流机场所获得的观测资料，给出了成都地区大气边界层的风速廓线。分析了辐射逆温的形成、发展和演变过程，及其精细结构。计算了离地面２米高处空气的变温率，结果表明，辐射逆温完全受地面长波辐射冷却和太阳辐射加热所控制。
Wind profiles of atmospheric boundary layer(ABL) are obtained from observations at Fenghuang Mountain and Shuangliu AirportThe formation and evolution process,and the fine structure of temperature inversion is analysis closelyThe changing rate of temperature at 2m height above the ground is computedIt is shown that radiation inversion is controled by the surface radiation cooling and the sun radiation heating
出处
《四川环境》
1998年第1期61-63,共3页
Sichuan Environment
