no-slip houiidaries in, 230. 231
numericil computation and methods in.
plume dispersion model of, 222
time scaler in, 220- 222
22s 236
Turbulent stable boundary layer, model of.
Turhulent transport
77 BX
coefficients in. 1x2 184
computational models of, 169~ 191
dissipation equations in, 172 175. 182
gradient models in, 25 54
high Reynolds number approrhation in.
mean field homogeneity condition in. 45
mean field time stationary condition in,
modeling of third moments in, 176.179
reversed kinetic energy transformation in.
ReynoldsiPeclet number order of signifiweak anisotropy in. 177
third moments in. 176- 179
Townsend’s data in. 186. 190
transport model for. 43 47
transport ternis in. I80 181
two-dimensionill isothermal wake in.
172- 175
45
42
cance in. 176
1x4 IYI
Turbulent v i s c q i t y coefficient, 8
Two-dimensional How
field equation for. 143- 144
simulation of turbulent diHusion for,
142 152
Two-dimensional isothermal wake, in
turhulent transport. IH4 191
Two-dimensional vorticity Acld. numerically
generated, 145
U
Unstable boundary layer
entrainment process in. I I S I 2 I
numerical integration procedure in,
thermodynamic model for, I I I - 123
similarity theories in, 133 136
surface layer of atmosphere in, I3 I I38
121-123
Unstable conditions
V
Velocity isoplcths, in channel flow, 155
Vertical mixing, in stahly stratified waters.
Vorticity field. numerically generated. 145
339-35 1
W
Wall turbulence
conditional akeraging analysis in. 154-259
experimental technique in. 251
prohubility density distributions in.
statistical analysis of. 249-260
Wave equation limit. in random walks, 35
Wave& wind-generated. 395- 397
Weak anisotropy, in turbulent transport, I77
Wicner-Hermite representation, for statistical
Windrows. floating pollution and. 372-377
253,260
turbuknce, 445 ~455
B 5
C 6
0 7
€ 8
F 9
G O
H 1
1 2
1 3