Modeling vertical heat transport in the wave affected surface layer of the ocean

Jinliang Wang; Jinbao Song

doi:10.1007/s00343-009-9133-z

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Modeling vertical heat transport in the wave affected surface layer of the ocean

OriginalPaper | Updated：2023-05-16

- Modeling vertical heat transport in the wave affected surface layer of the ocean
- Modeling vertical heat transport in the wave affected surface layer of the ocean
- 海洋湖沼学报（英文） 2009年27卷第2期页码：202-207
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Institute of Applied Mathematics College of Science Qingdao Technological University
  3. Key Laboratory of Ocean Circulation and Waves(KLOCAW) Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Supported by the National High Technology Research and Development Program of China (863 Program, No. 2006AA09A309);China Postdoctoral Science Foundation (No. 20070411111) and the Fund of Shandong Province for the Excellent Post-Doctors (No. 200603056)
- DOI：10.1007/s00343-009-9133-z
  中图分类号：
- 网络首发：2009-07-12，
  
  纸质出版：2009
- Accepted：
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Modeling vertical heat transport in the wave affected surface layer of the ocean[J]. 海洋湖沼学报（英文）, 2009,27(2):202-207.

Wang, J., Song, J. Modeling vertical heat transport in the wave affected surface layer of the ocean., Chin. J. Ocean. Limnol. 27, 202–207 (2009). https://doi.org/10.1007/s00343-009-9133-z
Modeling vertical heat transport in the wave affected surface layer of the ocean[J]. 海洋湖沼学报（英文）, 2009,27(2):202-207. DOI： 10.1007/s00343-009-9133-z.

Wang, J., Song, J. Modeling vertical heat transport in the wave affected surface layer of the ocean., Chin. J. Ocean. Limnol. 27, 202–207 (2009). https://doi.org/10.1007/s00343-009-9133-z DOI：

摘要

Abstract

In considering the vertical heat transport problems in the upper ocean

the flat upper boundary approximation for the free surface and the horizontal homogenous hypothesis are usually applied. However

due to the existence of the wave motion

the application of this approximation may result in some errors to the solar irradiation since it decays quickly in respect to the actual thickness of the water layer below the surface; on the other hand

due to the fluctuation of the water layer depth

it is improper to neglect the effects of the horizontal advection and turbulent diffusion since they also contribute to the vertical heat transport. A new model is constructed in this study to reflect these effects. The corresponding numerical simulations show that the wave motion may remarkably accelerate the vertical heat transferring process and the variation of the temperature in the wave affected layer appears in an oscillating manner.

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Keywords

references

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