Similarity in the Marine Atmospheric Surface Layer: The Role of Intermittency and Boundary-Layer Structures

1997 ◽  
Author(s):  
C. W. Fairall ◽  
R. J. Hill
2005 ◽  
Vol 116 (2) ◽  
pp. 237-252 ◽  
Author(s):  
G. J. Steeneveld ◽  
A. A. M. Holtslag ◽  
H. A. R. Debruin

MAUSAM ◽  
2021 ◽  
Vol 43 (3) ◽  
pp. 283-290
Author(s):  
S. SIVARAMAKRISHNAN

A system of Honeycomb Flat Plate (HFP) grid and cylindrical rods has been developed to accelerate the growth of a thick (32 cm) turbulent boundary layer, artificially, over rough floor of a low speed short test-section (0.61 m x 0.61 m) wind tunnel. Simulated profiles of wind velocity, longitudinal turbulence intensity and Reynolds stress are shown to have similarity to those of a neutral atmospheric boundary layer over a typical rural terrain. Longitudinal spectrum of turbulence measured at 10,30 and 100 mm above tunnel floor is shown to compare well with atmospheric spectrum and agree closely with the Kolmogoroff's -2/3 law in the inertial sub-range of the spectrum. Based on the length scale of longitudinal turbulence estimated from the spectrum, a scale of 1 :900 has been proposed for laboratory modeling of environmental problems wherein the transport of mass in a neutral atmospheric surface layer IS solely due to eddies of mechanical origin.


1978 ◽  
Vol 86 (3) ◽  
pp. 491-511 ◽  
Author(s):  
M. M. Gibson ◽  
B. E. Launder

Proposals are made for modelling the pressure-containing correlations which appear in the transport equations for Reynolds stress and heat flux in a simple way which accounts for gravitational effects and the modification of the fluctuating pressure field by the presence of a wall. The predicted changes in structure are shown to agree with Young's (1975) measurements in a free stratified shear flow and with the Kansas data on the atmospheric surface layer.


2017 ◽  
Vol 143 (706) ◽  
pp. 2182-2197 ◽  
Author(s):  
Kaighin A. McColl ◽  
Chiel C. van Heerwaarden ◽  
Gabriel G. Katul ◽  
Pierre Gentine ◽  
Dara Entekhabi

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