A numerical study of Stokes drift and thermal effects on the oceanic mixed layer

Xuewei Li; Dongliang Zhao; Zhongshui Zou

doi:10.1007/s13131-019-1448-9

Volume 39 Issue 5

May 2020

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Xuewei Li, Dongliang Zhao, Zhongshui Zou. A numerical study of Stokes drift and thermal effects on the oceanic mixed layer[J]. Acta Oceanologica Sinica, 2020, 39(5): 35-45. doi: 10.1007/s13131-019-1448-9

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Xuewei Li, Dongliang Zhao, Zhongshui Zou. A numerical study of Stokes drift and thermal effects on the oceanic mixed layer[J]. Acta Oceanologica Sinica, 2020, 39(5): 35-45. doi: 10.1007/s13131-019-1448-9

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A numerical study of Stokes drift and thermal effects on the oceanic mixed layer

doi: 10.1007/s13131-019-1448-9

Xuewei Li¹,
Dongliang Zhao^{1
,
,},
Zhongshui Zou^{2
,
,}

1.
Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, China
2.
Ocean College, Zhejiang University, Zhoushan 316021, China

Funds: The National Natural Science Foundation of China under contract Nos 41876010 and 41276015; the Public Science and Technology Research Funds Projects of Ocean under contrct No. 201505007; the Joint Project for the National Oceanographic Center by the NSFC and Shandong Government under contract No. U1406402; the National Natural Science Foundation of China under contract No. 41806028.

More Information

Corresponding author: E-mail: dlzhao2013@163.com; zouzhongshui@126.com
Received Date: 2019-05-28
Accepted Date: 2019-11-12

Available Online: 2020-12-28

Publish Date: 2020-05-25

Abstract

Abstract

This study explores the influence of Stokes drift and the thermal effects on the upper ocean bias which occurs in the summer with overestimated sea surface temperature (SST) and shallower mixed layer depth (MLD) using Mellor-Yamada turbulence closure scheme. The upper ocean thermal structures through Princeton ocean model are examined by experiments in the cases of idealized forcing and real observational situation. The results suggest that Stokes drift can generally enhance turbulence kinetic energy and deepen MLD either in summer or in winter. This effect will improve the simulation results in summer, but it will lead to much deeper MLD in winter compared to observational data. It is found that MLD can be correctly simulated by combining Stokes drift and the thermal effects of the cool skin layer and diurnal warm layer on the upper mixing layer. In the case of high shortwave radiation and weak wind speed, which usually occurs in summer, the heat absorbed from sun is blocked in the warm layer and prevented from being transferred downwards. As a result, the thermal effects in summer nearly has no influence on dynamic effect of Stokes drift that leads to deepening MLD. However, when the stratification is weak in winter, the thermal effects will counteract the dynamic effect of Stokes drift through enhancing the strength of stratification and suppress mixing impact. Therefore, the dynamic and thermal effects should be considered simultaneously in order to correctly simulate upper ocean thermal structures in both summer and winter.
- mixed layer,
- cool skin layer,
- diurnal warm layer,
- Stokes drift

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References(38)

References

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