TY - JOUR
T1 - A comparison of shear- and buoyancy-driven planetary boundary layer flows
AU - Chin-Hoh Moeng, Moeng
AU - Sullivan, P. P.
PY - 1994
Y1 - 1994
N2 - Planetary boundary layer (PBL) flows are known to exhibit fundamental differences depending on the relative combination of wind shear and buoyancy forces. Four large-eddy simulations (LESs) spanning the shear and buoyancy flow regimes were generated; two correspond to the extreme cases of shear and buoyancy-driven PBLs, while the other two represent intermediate PBLs where both forces are important. The extreme cases are used to highlight and quantify the basic differences between shear and convective PBLs in: 1) flow structures, 2) overall statistics, and 3) turbulent kinetic energy (TKE) budget distributions. Results from the two intermediate LES cases are used to develop and verify a velocity scaling and a TKE budget model, which are proposed for the intermediate PBL. -from Authors
AB - Planetary boundary layer (PBL) flows are known to exhibit fundamental differences depending on the relative combination of wind shear and buoyancy forces. Four large-eddy simulations (LESs) spanning the shear and buoyancy flow regimes were generated; two correspond to the extreme cases of shear and buoyancy-driven PBLs, while the other two represent intermediate PBLs where both forces are important. The extreme cases are used to highlight and quantify the basic differences between shear and convective PBLs in: 1) flow structures, 2) overall statistics, and 3) turbulent kinetic energy (TKE) budget distributions. Results from the two intermediate LES cases are used to develop and verify a velocity scaling and a TKE budget model, which are proposed for the intermediate PBL. -from Authors
UR - https://www.scopus.com/pages/publications/0028607746
U2 - 10.1175/1520-0469(1994)051<0999:acosab>2.0.co;2
DO - 10.1175/1520-0469(1994)051<0999:acosab>2.0.co;2
M3 - Article
AN - SCOPUS:0028607746
SN - 0022-4928
VL - 51
SP - 999
EP - 1022
JO - Journal of the Atmospheric Sciences
JF - Journal of the Atmospheric Sciences
IS - 7
ER -