作者: J. Weinstock
DOI: 10.1175/1520-0469(1978)035<1022:VTDIAS>2.0.CO;2
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摘要: Abstract The vertical turbulent diffusion coefficient in a stably stratified fluid is derived analytically. This derivation does not require that the flux Richardson number be known or specified. resulting expression for compared with previous stratospheric results of Lilly et al. (1974) and its applicability to atmospheric clear air turbulence discussed.