摘要
基于2005年盘锦芦苇湿地近地面层湍流通量和微气象梯度的连续观测,研究了芦苇湿地近地面层湍流通量参数化方案。结果表明:盘锦芦苇湿地近地面层经常维持弱稳定和弱不稳定层结。在不稳定层结(-0.4<z/L<-0.01)时,盘锦芦苇湿地近地面层湍流通量计算可采用Businger-Dyer稳定度方案,在此稳定度范围之外B-D方案的适用性需要进一步验证。
Based on the turbulent flux data in atmospheric surface layer from eddy covariance tower and micrometeorological gradient data in 2005 in reed wetland of Panjin,parameterization scheme of turbulent flux was discussed.The results indicate that the atmospheric stability in atmospheric surface layer of reed wetland often maintains weakly stable or unstable stratification.Businger-Dyer stability function parameter scheme could be used to calculate turbulent flux in this region under unstable stratification（-0.4〈z/L〈-0.1）,otherwise the parameterization scheme should be tested beyond this ranges as mentioned above.
出处
《气象与环境学报》
2009年第5期7-12,共6页
Journal of Meteorology and Environment
基金
国家杰出青年科学基金项目(40625015)
国家重点基础研究发展规划项目(2004CB418507-1)共同资助
关键词
芦苇湿地
湍流通量
参数化方案
涡度相关
微气象梯度
Reed wetland
Turbulent flux
Parameterization scheme
Eddy covariance
Micrometeorological gradient
