Contribution of wind shear to the entrainment process of the atmospheric convective boundary layer

Contribution of wind shear to the entrainment process of the atmospheric convective boundary layer
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风切变对大气对流边界层夹带过程的贡献

DOI:
10.3319/tao.2020.02.11.01
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发表时间:
2020
期刊:
Terr. Atmos. Ocean. Sci.
影响因子:
--
通讯作者:
刘滔
刘滔
中科院分区:
其他
文献类型:
--
作者:
李岸然;高文峰;刘滔

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Wind shear induced by the velocity difference has an important effect on the stably stratified turbulent flow in the atmospheric convective boundary layer (CBL). Cases with different velocity difference are conducted by Large-eddy simulation (LES) to reveal the contribution of shear effect to entrainment. The result shows that the shear-generated turbulent kinetic energy (TKE) in the entrainment layer is partially consumed by the negative buoyancy, which increases the entrainment flux minimum and enhances the entrainment flux ratio in the range of 0.188 0.352. Based on the hypothesis of the independence of the shear-generated TKE and buoyancygenerated TKE, an approach for the fraction of the shear-generated TKE available for entrainment is proposed, and the averaged fraction reaches 38.5%, but the evolution tends to increase with the enlargement of velocity difference. Article history: Received 24 September 2019 Revised 10 December 2019 Accepted 11 February 2020
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