caa a22 4500 46908457X CHVBK 20180323133001.0 cr unu---uuuuu 170328e19920601xx s 000 0 eng 10.1007/BF02657505 doi (NATIONALLICENCE)springer-10.1007/BF02657505 Effects of turbulent dispersion of atmospheric balance motions of planetary boundary layer [Elektronische Daten] [Liu Shikuo, Huang Wei, Rong Pingping] New Reynolds' mean momentum equations including both turbulent viscosity and dispersion are used to analyze atmospheric balance motions of the planetary boundary layer. It is pointed out that turbulent dispersion with γ 0 will increase depth of Ekman layer, reduce wind velocity in Ekman layer and produce a more satisfactory Ekman spiral lines fit the observed wind hodograph. The wind profile in the surface layer including turbulent dispersion is still logarithmic but the von Karman constantk is replaced byk 1 = √ 1 —k/2, the wind increases a little more rapidly with height. Advances in Atmospheric Sciences, 1992 Shikuo Liu Department of Geophysics, Peking University, 100871, Beijing aut Wei Huang Department of Geophysics, Peking University, 100871, Beijing aut Pingping Rong Department of Geophysics, Peking University, 100871, Beijing aut Advances in Atmospheric Sciences Science Press 9/2(1992-06-01), 147-156 0256-1530 9:2<147 1992 9 376 https://doi.org/10.1007/BF02657505 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF02657505 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Shikuo Liu Department of Geophysics, Peking University, 100871, Beijing aut NATIONALLICENCE 700 1- Wei Huang Department of Geophysics, Peking University, 100871, Beijing aut NATIONALLICENCE 700 1- Pingping Rong Department of Geophysics, Peking University, 100871, Beijing aut NATIONALLICENCE 773 0- Advances in Atmospheric Sciences Science Press 9/2(1992-06-01), 147-156 0256-1530 9:2<147 1992 9 376 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer