Javascript must be enabled to continue!
Characteristics of the secondary circulations in the convective boundary layer over two-dimensional heterogeneous surfaces
View through CrossRef
<p>Large-eddy simulations are performed to investigate the effects of background wind on the secondary circulations (SCs) in the convective boundary layer. Heterogeneities are produced by a prescribed two-dimensional surface sensible heat flux pattern of chessboard-type and have a size which is a bit larger than the boundary layer height.</p><p>When the wind blows along the diagonal of the chessboard-like pattern, the roll-like SCs are observed even when the background wind speed is as large as 10m/s, with whose axes are oriented along the diagonal of the pattern. Another case with wind direction along neither the diagonal nor the side of the chessboard-like pattern and weak wind speed shows the roll-like SCs still exist but lack symmetry. The SCs become much weaker and change their axes orientation when the wind speed increases.</p><p>Meanwhile, the results are different when the Coriolis force is considered. When the background wind is weak, the asymmetry of the SCs become more significant with the development of boundary layer when the Coriolis force is considered, while the SCs tend to be symmetrical without the Coriolis force. When the background wind strengthens, the SCs are more difficult to maintain in the case of Coriolis force.</p><p>Further analysis through rotational and divergent decomposition suggests which part contributes more to the maintenance of the SCs.</p><p></p>
Title: Characteristics of the secondary circulations in the convective boundary layer over two-dimensional heterogeneous surfaces
Description:
<p>Large-eddy simulations are performed to investigate the effects of background wind on the secondary circulations (SCs) in the convective boundary layer.
Heterogeneities are produced by a prescribed two-dimensional surface sensible heat flux pattern of chessboard-type and have a size which is a bit larger than the boundary layer height.
</p><p>When the wind blows along the diagonal of the chessboard-like pattern, the roll-like SCs are observed even when the background wind speed is as large as 10m/s, with whose axes are oriented along the diagonal of the pattern.
Another case with wind direction along neither the diagonal nor the side of the chessboard-like pattern and weak wind speed shows the roll-like SCs still exist but lack symmetry.
The SCs become much weaker and change their axes orientation when the wind speed increases.
</p><p>Meanwhile, the results are different when the Coriolis force is considered.
When the background wind is weak, the asymmetry of the SCs become more significant with the development of boundary layer when the Coriolis force is considered, while the SCs tend to be symmetrical without the Coriolis force.
When the background wind strengthens, the SCs are more difficult to maintain in the case of Coriolis force.
</p><p>Further analysis through rotational and divergent decomposition suggests which part contributes more to the maintenance of the SCs.
</p><p></p>.
Related Results
The vertical distribution of PM2.5 and boundary-layer structure during winter haze in Nanjing
The vertical distribution of PM2.5 and boundary-layer structure during winter haze in Nanjing
<p>At the end of November 2018, a heavy air pollution event was recorded by many meteorological stations in the Yangtze River Delta (YRD), China. The local PM2.5 conc...
Penetrative convection in Nocturnal ABL: Numerical Simulations
Penetrative convection in Nocturnal ABL: Numerical Simulations
<p>After the sunset, under calm and clear sky conditions, aerosol laden surface air-layer, cools rapidly due to radiative cooling<sup>[1, 2, & 3...
On the Formulation of Nonreflecting Boundary Conditions for Turbomachinery Configurations: Part II — Application and Analysis
On the Formulation of Nonreflecting Boundary Conditions for Turbomachinery Configurations: Part II — Application and Analysis
Abstract
The flow in turbomachinery components is complex due to the relative motion of rotating and non-rotating elements. A proper design and prediction of physica...
Atmospheric Convection
Atmospheric Convection
Abstract
This graduate-level meteorology text and reference provides a scientifically rigorous description of the many types of convective circulations in the Earth'...
Tracer measurements in the tropical tropopause layer during the AMMA/SCOUT-O3 aircraft campaign
Tracer measurements in the tropical tropopause layer during the AMMA/SCOUT-O3 aircraft campaign
Abstract. We present airborne in situ measurements made during the AMMA (African Monsoon Multidisciplinary Analysis)/SCOUT-O3 campaign between 31 July and 17 August 2006 on board t...
On the Formulation of Nonreflecting Boundary Conditions for Turbomachinery Configurations: Part I — Theory and Implementation
On the Formulation of Nonreflecting Boundary Conditions for Turbomachinery Configurations: Part I — Theory and Implementation
Abstract
With unsteady flow simulations of industrial turbomachinery configurations becoming more and more affordable there is a growing need for accurate inlet and ...
Research Progress on Superhydrophobic Surface Preparation Methods and Mechanical Durability
Research Progress on Superhydrophobic Surface Preparation Methods and Mechanical Durability
:
Superhydrophobic surfaces have great application prospects due to their unique surface-
wetting characteristics. However, superhydrophobic surfaces' micro-nano binary rough struc...
Analysis of a server convective rainstorm in the weak background
Analysis of a server convective rainstorm in the weak background
<p>Using conventional and unconventional meteorological observation dataes, RMAPS-NOW( RR4DVar cloud model), the severe convective rainstorm occurred over the Beijing...

