Second-Order Modeling Of Turbulent Diffusion in an Atmospheric Surface Layer

1992 ◽  
pp. 39-58 ◽  
Author(s):  
V. M. Tsarenko ◽  
A. M. Yaglom
Keyword(s):  
Surface Layer ◽  
Turbulent Diffusion ◽  
Atmospheric Surface Layer ◽  
Second Order

Semiempirical theories of turbulent diffusion in an atmospheric surface layer

1991 ◽  
Vol 3 (5) ◽  
pp. 1448-1448
Author(s):  
V. M. Tsarenko ◽  
A. M. Yaglom
Keyword(s):  
Surface Layer ◽  
Turbulent Diffusion ◽  
Atmospheric Surface Layer

Probability law of turbulent kinetic energy in the atmospheric surface layer

2021 ◽  
Vol 6 (7) ◽  
Author(s):  
Mohammad Allouche ◽  
Gabriel G. Katul ◽  
Jose D. Fuentes ◽  
Elie Bou-Zeid
Keyword(s):  
Surface Layer ◽  
Kinetic Energy ◽  
Turbulent Kinetic Energy ◽  
Atmospheric Surface Layer

scholarly journals The surface layer integral method for the modelling of the radial gravity gradient component over sea surface

2019 ◽  
Vol 9 (1) ◽  
pp. 127-132
Author(s):  
D. Zhao ◽  
Z. Gong ◽  
J. Feng
Keyword(s):  
Surface Layer ◽  
Integral Method ◽  
Integral Formula ◽  
Radial Component ◽  
Second Order ◽  
Sea Surface ◽  
Gravity Potential ◽  
Gravity Gradient ◽  
Disturbing Potential ◽  
Gradient Component

Abstract For the modelling and determination of the Earth’s external gravity potential as well as its second-order radial derivatives in the space near sea surface, the surface layer integral method was discussed in the paper. The reasons for the applicability of the method over sea surface were discussed. From the original integral formula of disturbing potential based on the surface layer method, the expression of the radial component of the gravity gradient tensor was derived. Furthermore, an identity relation was introduced to modify the formula in order to reduce the singularity problem. Numerical experiments carried out over the marine area of China show that, the modi-fied surface layer integral method effectively improves the accuracy and reliability of the calculation of the second-order radial gradient component of the disturbing potential near sea surface.

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