Journal of Tropical Oceanography ›› 2021, Vol. 40 ›› Issue (3): 57-68.doi: 10.11978/YG2020005CSTR: 32234.14.YG2020005

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On the mechanisms behind diurnal variations in air-sea turbulent heat fluxes under different boundary layer stability

XU Changsan1,2(), SONG Xiangzhou2(), QI Yiquan2   

  1. 1. Nantong Marine Environmental Monitoring Center, State Oceanic Administration, Natong 226002, China
    2. Key Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing 210024, China
  • Received:2020-11-11 Revised:2021-01-12 Online:2021-05-10 Published:2021-01-26
  • Contact: SONG Xiangzhou E-mail:xcs0576@126.com;xzsong@hhu.edu.cn
  • Supported by:
    National Natural Science Foundation of China(42076016)

Abstract:

The air-sea turbulent heat fluxes (THFs), including the evaporative latent heat flux and convective sensible heat flux, are key components in air-sea interaction and ocean circulation, which are important for our understanding of the global energy balance, water cycle and climate change. Due to the limitations of observations and numerical simulations, the diurnal variations in THFs are however not accurately known. In this paper, we propose a future research plan toward identifying the mechanisms behind diurnal variations in THFs. With the recent development of traditional buoy observations, new observations (e.g., glider) and newly released atmospheric reanalysis, it is helpful to research the diurnal variations in THFs. Using the combined observations and reanalysis, we investigate the key scientific issues on diurnal variations in THFs under different boundary layer stability based on the bulk formulas and turbulence methods. In the future, we will demonstrate the global basic structures and dominant factors for diurnal variations in THFs, as well as the strength of the diurnal variation associated with the extreme weather processes and climate events. To evaluate accurate magnitudes of THFs for better understanding of diurnal variations, high-frequency surface currents and height-dependent air-sea physical variables will be incorporated into the estimates of THFs in terms of bulk formulas. Innovatively, this study transfers the multi-scale THF variations into the space of boundary layer stability to concentrate on the diurnal variations, which help study the mixed-layer dynamics, upper-ocean ecosystems, energy balance, and climate change.

Key words: air-sea turbulent heat fluxes, diurnal variation, boundary layer stability, buoy observation, surface current

CLC Number: 

  • P732.6