Solitary Wave-Turbulence Interaction in the Stable Atmospheric Boundary Layer

1995 ◽  
pp. 122-126
Author(s):  
Neil Edwards ◽  
Stephen Mobbs
Keyword(s):  
Boundary Layer ◽  
Solitary Wave ◽  
Atmospheric Boundary Layer ◽  
Wave Turbulence ◽  
Stable Atmospheric Boundary Layer

scholarly journals Review of wave‐turbulence interactions in the stable atmospheric boundary layer

2015 ◽  
Vol 53 (3) ◽  
pp. 956-993 ◽  
Author(s):  
Jielun Sun ◽  
Carmen J. Nappo ◽  
Larry Mahrt ◽  
Danijel Belušić ◽  
Branko Grisogono ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Atmospheric Boundary Layer ◽  
Wave Turbulence ◽  
Stable Atmospheric Boundary Layer

scholarly journals Spatiotemporal Dynamics of the Kinetic Energy in the Atmospheric Boundary Layer from Minisodar Measurements

Atmosphere ◽  
2021 ◽  
Vol 12 (4) ◽  
pp. 421
Author(s):  
Alexander Potekaev ◽  
Liudmila Shamanaeva ◽  
Valentina Kulagina
Keyword(s):  
Boundary Layer ◽  
Kinetic Energy ◽  
Atmospheric Boundary Layer ◽  
Turbulent Kinetic Energy ◽  
Time Of Day ◽  
Linear Increase ◽  
Spatiotemporal Dynamics ◽  
Intermediate Layers ◽  
Subsequent Decrease ◽  
Stable Atmospheric Boundary Layer

Spatiotemporal dynamics of the atmospheric kinetic energy and its components caused by the ordered and turbulent motions of air masses are estimated from minisodar measurements of three velocity vector components and their variances within the lowest 5–200 m layer of the atmosphere, with a particular emphasis on the turbulent kinetic energy. The layered structure of the total atmospheric kinetic energy has been established. From the diurnal hourly dynamics of the altitude profiles of the turbulent kinetic energy (TKE) retrieved from minisodar data, four layers are established by the character of the altitude TKE dependence, namely, the near-ground layer, the surface layer, the layer with a linear TKE increase, and the transitive layer above. In the first layer, the most significant changes of the TKE were observed in the evening hours. In the second layer, no significant changes in the TKE values were observed. A linear increase in the TKE values with altitude was observed in the third layer. In the fourth layer, the TKE slightly increased with altitude and exhibited variations during the entire observation period. The altitudes of the upper boundaries of these layers depended on the time of day. The MKE values were much less than the corresponding TKE values, they did not exceed 50 m2/s2. From two to four MKE layers were distinguished based on the character of its altitude dependence. The two-layer structures were observed in the evening and at night (under conditions of the stable atmospheric boundary layer). In the morning and daytime, the four-layer MKE structures with intermediate layers of linear increase and subsequent decrease in the MKE values were observed. Our estimates demonstrated that the TKE contribution to the total atmospheric kinetic energy considerably (by a factor of 2.5–3) exceeded the corresponding MKE contribution.

Multiple master length scales for stable atmospheric boundary layer

1992 ◽  
Vol 15 (4) ◽  
pp. 409-416 ◽  
Author(s):  
G. A. Degrazia ◽  
A. P. de Oliveira ◽  
J. Goedert
Keyword(s):  
Boundary Layer ◽  
Atmospheric Boundary Layer ◽  
Length Scales ◽  
Stable Atmospheric Boundary Layer
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