SlJRJECT INIXX
459
Kramers-Moyal expansloti. 34
K-theor) model, 170. 1x1
L
Lagrnngian autocorrelation. ('orrrin
hypothesis and. I49 I52
I.agrangian equations, for diffusion in
stationary isotropic field. 146 149
Lagrangian-Eulerian time-scale relationship
for balloon flights, 419~ 430
variations rrom wind speed in. 426 429
Lagrangian-Eulerian vert ical-velocity
Lagrangian field, generation of, I46
Lagrangian information. in threedimensional calculation, 156- I W
Liigrangian quantities, particle triijcctories
and. 157
L.aprangian Reynolds stress. 140
Lagrangian turbulence, two-particle
Lagrangian turbulent quantitics. numcrical
I angniuir circulation
spectra. 422 423
\eparation in. 152
vmuliition 01. 141 102
diflusive power of, 31 I
floating pollutants and. 372 373
li I t c red moment u ni a nil con t I iiu it y
numerical simulation 111. 23X
Large-cdtlq wnulation
equations in. 13g 241
Liirgc-scale turbulence. energy loss in.
Lateral diffusion, from source at sea, 316-321
Length scales, in turbulent shear flow,
241 246
2 I h.-2 I H
Monientum. turbulent diffusion of in ocean.
Momentumless wahe. in turbulent shear
342 360
now. 232 z3.l
N
Navier-Stokes cquations. 3- 4. 15, 63
in Lagranpian turbulence. I53
in turhulent shear flow, 225 226
Wiener-Hermite statistical turbulence and.
445
North Sea. turbidity diffusion in. 331- 337
No-slip boundary, in turhulent shear flow.
230 231
OGed I1
electronic circuits fcjr lurhulence signals
heat measurement in. 355 3M
Cromwell current in. 360 361
interactions of with atmohphcre. 391 404
mixed layers in. 364 361
surface icmperature diatrihution in.
turbulence sources for, 360
turbulent diflusion of heat and momentum
universal similarity theory for. 35.5 35X
Ocean suiface waves. turhulrnce generation
in. 3.58 359
31s 388
in. 353. 369
by, 368 369
I'
Particle statistics. for arbitrary P. Q. 66
Peclct numher. dcnsity interhccs and.
Planetary boundary layer
haroclinic cases in. 412
barotropic. 410 412
edd) ditrusion cocfficienr in. 407 417
Icngth of mixed layer in. 73 01
maximum ground cnnccntriititm error in,
nonstationarity of. 413 31 7
441 443
416 417
459
Kramers-Moyal expansloti. 34
K-theor) model, 170. 1x1
L
Lagrnngian autocorrelation. ('orrrin
hypothesis and. I49 I52
I.agrangian equations, for diffusion in
stationary isotropic field. 146 149
Lagrangian-Eulerian time-scale relationship
for balloon flights, 419~ 430
variations rrom wind speed in. 426 429
Lagrangian-Eulerian vert ical-velocity
Lagrangian field, generation of, I46
Lagrangian information. in threedimensional calculation, 156- I W
Liigrangian quantities, particle triijcctories
and. 157
L.aprangian Reynolds stress. 140
Lagrangian turbulence, two-particle
Lagrangian turbulent quantitics. numcrical
I angniuir circulation
spectra. 422 423
\eparation in. 152
vmuliition 01. 141 102
diflusive power of, 31 I
floating pollutants and. 372 373
li I t c red moment u ni a nil con t I iiu it y
numerical simulation 111. 23X
Large-cdtlq wnulation
equations in. 13g 241
Liirgc-scale turbulence. energy loss in.
Lateral diffusion, from source at sea, 316-321
Length scales, in turbulent shear flow,
241 246
2 I h.-2 I H
Monientum. turbulent diffusion of in ocean.
Momentumless wahe. in turbulent shear
342 360
now. 232 z3.l
N
Navier-Stokes cquations. 3- 4. 15, 63
in Lagranpian turbulence. I53
in turhulent shear flow, 225 226
Wiener-Hermite statistical turbulence and.
445
North Sea. turbidity diffusion in. 331- 337
No-slip boundary, in turhulent shear flow.
230 231
OGed I1
electronic circuits fcjr lurhulence signals
heat measurement in. 355 3M
Cromwell current in. 360 361
interactions of with atmohphcre. 391 404
mixed layers in. 364 361
surface icmperature diatrihution in.
turbulence sources for, 360
turbulent diflusion of heat and momentum
universal similarity theory for. 35.5 35X
Ocean suiface waves. turhulrnce generation
in. 3.58 359
31s 388
in. 353. 369
by, 368 369
I'
Particle statistics. for arbitrary P. Q. 66
Peclct numher. dcnsity interhccs and.
Planetary boundary layer
haroclinic cases in. 412
barotropic. 410 412
edd) ditrusion cocfficienr in. 407 417
Icngth of mixed layer in. 73 01
maximum ground cnnccntriititm error in,
nonstationarity of. 413 31 7
441 443
416 417