EGU2020-12391
https://doi.org/10.5194/egusphere-egu2020-12391
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Characteristics of the secondary circulations in the convective boundary layer over two-dimensional heterogeneous surfaces

Zixuan Xiang, Jianning Sun, and Jun Zou
Zixuan Xiang et al.
  • School of Atmospheric Sciences, Nanjing University, Nanjing, China(dg1828014@smail.nju.edu.cn)

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.

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.

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.

Further analysis through rotational and divergent decomposition suggests which part contributes more to the maintenance of the SCs.

How to cite: Xiang, Z., Sun, J., and Zou, J.: Characteristics of the secondary circulations in the convective boundary layer over two-dimensional heterogeneous surfaces, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12391, https://doi.org/10.5194/egusphere-egu2020-12391, 2020

This abstract will not be presented.