TY - JOUR
T1 - Turbulence in the Stable Boundary Layer at Higher Richardson Numbers
AU - FERRERO, Enrico
AU - LH, Quan
AU - Massone, D.
PY - 2011
Y1 - 2011
N2 - We present some algebraic and numerical simulations of the stable boundary layer. We also discuss the problem of the existence of a critical Richardson number (Ri), beyond which the turbulence is suppressed. We compare the results of a second-order algebraic model with those of a third-order numerical model and, to this purpose, numerical simulations of a wind-tunnel flow, which is characterized by various Richardson numbers, were performed. As far as the second-order model is concerned, solutions, for the Richardson number greater than any critical value, can be obtained by modifying the time scales of the second-order equation pressure correlation terms in order to account for a buoyancy damping factor. We show that using a third-order model allows the same results (no critical Richardson number) to be obtained without modifications to the time scales. It is suggested that the non-locality, accounted for by the third-order moments, could allow the turbulence to persist also for Ri> 1.
AB - We present some algebraic and numerical simulations of the stable boundary layer. We also discuss the problem of the existence of a critical Richardson number (Ri), beyond which the turbulence is suppressed. We compare the results of a second-order algebraic model with those of a third-order numerical model and, to this purpose, numerical simulations of a wind-tunnel flow, which is characterized by various Richardson numbers, were performed. As far as the second-order model is concerned, solutions, for the Richardson number greater than any critical value, can be obtained by modifying the time scales of the second-order equation pressure correlation terms in order to account for a buoyancy damping factor. We show that using a third-order model allows the same results (no critical Richardson number) to be obtained without modifications to the time scales. It is suggested that the non-locality, accounted for by the third-order moments, could allow the turbulence to persist also for Ri> 1.
UR - https://iris.uniupo.it/handle/11579/15608
U2 - 10.1007/s10546-010-9581-1
DO - 10.1007/s10546-010-9581-1
M3 - Article
SN - 0006-8314
VL - 139
SP - 225
EP - 240
JO - Boundary-Layer Meteorology
JF - Boundary-Layer Meteorology
IS - 2
ER -