Direct numerical simulation of turbulent heat transfer across a sheared wind-driven gas-liquid interface

被引:15
作者
Kurose, Ryoichi [1 ,2 ]
Takagaki, Naohisa [1 ,2 ]
Kimura, Atsushi [1 ,2 ]
Komori, Satoru [1 ,2 ]
机构
[1] Kyoto Univ, Dept Mech Engn & Sci, Nishikyo Ku, Kyoto 6158140, Japan
[2] Kyoto Univ, Adv Res Inst Fluid Sci & Engn, Nishikyo Ku, Kyoto 6158140, Japan
关键词
air/sea interactions; gas/liquid flow; geophysical and geological flows; MASS-TRANSFER; LABORATORY MEASUREMENTS; BOUNDARY-LAYER; SENSIBLE HEAT; WATER-VAPOR; FLOW; FLUXES; GENERATION; EXCHANGE; MOBILE;
D O I
10.1017/jfm.2016.554
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Turbulent heat transfer across a sheared wind-driven gas-liquid interface is investigated by means of a direct numerical simulation of gas-liquid two-phase turbulent flows under non-breaking wave conditions. The wind-driven wavy gas-liquid interface is captured using the arbitrary Lagrangian-Eulerian method with boundary-fitted coordinates on moving grids, and the temperature fields on both the gas and liquid sides, and the humidity field on the gas side are solved. The results show that although the distributions of the total, latent, sensible and radiative heat fluxes at the gas-liquid interface exhibit streak features such that low-heat-flux regions correspond to both low-streamwise-velocity regions on the gas side and high-streamwise-velocity regions on the liquid side, the similarity between the heat-flux streak and velocity streak on the gas side is more significant than that on the liquid side. This means that, under the condition of a fully developed wind-driven turbulent field on both the gas and liquid sides, the heat transfer across the sheared wind-driven gas-liquid interface is strongly affected by the turbulent eddies on the gas side, rather than by the turbulent eddies and Langmuir circulations on the liquid side. This trend is quite different from that of the mass transfer (i.e. CO2 gas). This is because the resistance to heat transfer is normally lower than the resistance to mass transfer on the liquid side, and therefore the heat transfer is controlled by the turbulent eddies on the gas side. It is also verified that the predicted total heat, latent heat, sensible heat and enthalpy transfer coefficients agree well with previously measured values in both laboratory and field experiments. To estimate the heat transfer coefficients on both the gas and liquid sides, the surface divergence could be a useful parameter, even when Langmuir circulations exist.
引用
收藏
页码:646 / 687
页数:42
相关论文
共 64 条
  • [51] THE CHARACTERISTICS OF LOW-SPEED STREAKS IN THE NEAR-WALL REGION OF A TURBULENT BOUNDARY-LAYER
    SMITH, CR
    METZLER, SP
    [J]. JOURNAL OF FLUID MECHANICS, 1983, 129 (APR) : 27 - 54
  • [52] Simulation of turbulent flow over idealized water waves
    Sullivan, PP
    McWilliams, JC
    Moeng, CH
    [J]. JOURNAL OF FLUID MECHANICS, 2000, 404 : 47 - 85
  • [53] Takagaki N., 2016, IOP Conference Series: Earth and Environmental Science, V35, DOI 10.1088/1755-1315/35/1/012009
  • [54] Takagaki N., 2009, THESIS
  • [55] Effects of turbulent eddies and Langmuir circulations on scalar transfer in a sheared wind-driven liquid flow
    Takagaki, Naohisa
    Kurose, Ryoichi
    Tsujimoto, Yuta
    Komori, Satoru
    Takahashi, Keiko
    [J]. PHYSICS OF FLUIDS, 2015, 27 (01)
  • [56] Strong correlation between the drag coefficient and the shape of the wind sea spectrum over a broad range of wind speeds
    Takagaki, Naohisa
    Komori, Satoru
    Suzuki, Naoya
    Iwano, Koji
    Kuramoto, Takenori
    Shimada, Satoshi
    Kurose, Ryoichi
    Takahashi, Keiko
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2012, 39
  • [57] Tetens O., 1930, Zeitschrift fr Geophysik, V6, P297, DOI DOI 10.1016/J.FOODCHEM.2008.07.023
  • [58] Langmuir circulation
    Thorpe, SA
    [J]. ANNUAL REVIEW OF FLUID MECHANICS, 2004, 36 : 55 - 79
  • [59] Toba Y, 1972, J OCEANOGR SOC JAPAN, V28, P109, DOI [DOI 10.1007/BF02109772, 10.1007/BF02109772]
  • [60] Characteristics of interfacial signatures on a wind-driven gravity-capillary wave
    Tsai, Wu-ting
    Chen, Shi-ming
    Lu, Guan-hung
    Garbe, Christoph S.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2013, 118 (04) : 1715 - 1735