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   上混合层深度 在 海洋学 分类中 的翻译结果: 查询用时:0.089秒
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上混合层深度
相关语句
  mixed layer depth
    APPLICATION OF THE SIMILARITY THEORY TO FORECASTING THE UPPER MIXED LAYER DEPTH INOCEANS
    相似理论在海洋上混合层深度预报中的应用
短句来源
    The results show that the TKE model can simulate the main features of the time variation of the SST and mixed layer depth except in the middle period of May. In May and June, the diurnal oscillation of the SST is mainly determined by the diurnal variation of solar short-wave radiation, and the mixing effect of the wind restrains the diurnal oscillation of the SST in the south of the SCS.
    结果表明 :TKE模式能够模拟南海南部的海表面温度 SST以及除南海南部 5月中旬以外的上混合层深度随时间变化基本特征。 在 5~ 6月 ,SST的日振荡主要依赖于短波辐射的日变化 ,风的混合作用抑制了 SST的日周期振荡。
短句来源
    The results show that the TKE model can simulate the main features of the time variables of the SST and mixed layer depth.
    结果表明 ,TKE模式能够很好地模拟南海北部的海表面温度SST和上混合层深度随时间变化基本特征。
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  mixed layer depth
When the surface heat flux is balanced by a cross-shore heat flux, the surface mixed layer depth obtained from the WM model (Weatherly and Martin, 1978), hPRT, is roughly the same as observed.
      
The mixed layer depth calculated from the PWP model (Price, Weller and Pinkel, 1986) is close to the depth obtained from thermistor chain temperature data.
      
There is a clear relationship between upper mixed layer depth and wind-stress magnitude at subtidal frequencies.
      
Typically, the surface mixed layer depth lags the wind stress by 6-12 h.
      
The influence of westerly burst and rainfall on SST, salinity and mixed layer depth are discussed.
      
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  upper mixed layer depth
There is a clear relationship between upper mixed layer depth and wind-stress magnitude at subtidal frequencies.
      
Comparison of monthly upper mixed layer depth (MLD) and critical depth supported the possibility of the mismatch phenomenon.
      
  upper mixed layer depth
There is a clear relationship between upper mixed layer depth and wind-stress magnitude at subtidal frequencies.
      
Comparison of monthly upper mixed layer depth (MLD) and critical depth supported the possibility of the mismatch phenomenon.
      


In this paper, the one dimensional turbulence kinetic (TKE) model is used to simulate and do some experiments on the SST and the upper mixed layer in the south of the South China Sea (SCS). The results show that the TKE model can simulate the main features of the time variation of the SST and mixed layer depth except in the middle period of May. In May and June, the diurnal oscillation of the SST is mainly determined by the diurnal variation of solar short-wave radiation, and the mixing effect of the wind restrains...

In this paper, the one dimensional turbulence kinetic (TKE) model is used to simulate and do some experiments on the SST and the upper mixed layer in the south of the South China Sea (SCS). The results show that the TKE model can simulate the main features of the time variation of the SST and mixed layer depth except in the middle period of May. In May and June, the diurnal oscillation of the SST is mainly determined by the diurnal variation of solar short-wave radiation, and the mixing effect of the wind restrains the diurnal oscillation of the SST in the south of the SCS. Compared with solar short-wave radiation and the wind stress, the latent heat and sensible heat fluxes are a minor factor in controlling the variation of the SST and the mixed layer during summer monsoon onset in the SCS. Solar short wave radiation is the main heat source to maintain the SST. In spring, the effect of short-wave radiation could make the SST in the south of the SCS increase 4℃ or less; and latent heat and sensible heat fluxes could make the SST decrease 3℃. The wind controls the depth of the upper mixed layer, and its effect could make the mixed layer grow 20~30 m, the short-wave radiation could make the mixed layer shallow 2~3 m and the latent heat and sensible heat fluxes make the mixed layer become 1~2 m deeper. In the south of the SCS the effect of heat fluxes on the mixed layer depth is smaller than the effect of wind in spring.

采用一维湍动能模式对南海南部的 SST及混合层进行数值模拟和数值试验。结果表明 :TKE模式能够模拟南海南部的海表面温度 SST以及除南海南部 5月中旬以外的上混合层深度随时间变化基本特征。在 5~ 6月 ,SST的日振荡主要依赖于短波辐射的日变化 ,风的混合作用抑制了 SST的日周期振荡。春季夏季风爆发期间 ,南海海面潜热通量和感热通量与短波辐射和风应力相比较 ,是一个对 SST和混合层影响较小的量。在春季南海南部 ,短波辐射作用能使 SST升高的最大值约为 4℃ ;潜热和感热通量能使 SST的下降的最大值为 3℃。风应力对南海混合层深度随时间变化趋势起着决定的作用 ,并能使其深度加深 2 0~ 30 m,而短波辐射则使混合层的深度变浅2~ 3m,潜热和感热通量会使混合层的深度加深 1~ 2 m。在春季南海南部 ,热通量对混合层深度的影响与风应力相比要小得多

In this paper, a 1 D Turbulence Kinetic Energy (TKE) model was used to simulate and experiment on the SST and upper mixed layer in the northern South China Sea ( SCS ) in spring, and to discuss the relevant mechanisms. The results show that the TKE model can simulate the main features of the time variables of the SST and mixed layer depth. In May and June, 1998, the daily oscillation of the SST was mainly determined by daily variation of the solar short wave radiation, which maintained the ...

In this paper, a 1 D Turbulence Kinetic Energy (TKE) model was used to simulate and experiment on the SST and upper mixed layer in the northern South China Sea ( SCS ) in spring, and to discuss the relevant mechanisms. The results show that the TKE model can simulate the main features of the time variables of the SST and mixed layer depth. In May and June, 1998, the daily oscillation of the SST was mainly determined by daily variation of the solar short wave radiation, which maintained the SST mainly and caused the SST increase by 1-4℃; the mixing effect of the wind restrained the daily oscillation of the SST . Compared with solar short wave radiation and wind stress, the latent heat and sensible heat flux are a minor factor in controlling the variable of the SST in spring. In May, both wind stress and solar short wave radiation control the depth of the upper mixed layer, and the effect of wind stress caused the mixed layer to grow to 5-10m, and the short wave radiation could reduce the mixed layer depth by 5-10m. However, in June, solar short wave radiation was smaller after summer monsoon onset, reducing the mixed layer depth only by 1-2m, and the latent heat and sensible heat flux further enhanced the mixed layer depth by more than 1-2m, with the depth of mixed layer being controlled mainly by wind stress.

根据 1 998年南海季风实验 (SCSMEX)北部“实验 3号”调查船的观测资料 ,采用一维湍动能模式 (TKE模式 ) ,对春季南海北部的SST及混合层随时间变化特征进行了数值模拟和数值试验。结果表明 ,TKE模式能够很好地模拟南海北部的海表面温度SST和上混合层深度随时间变化基本特征。在南海 5— 6月 ,SST的日振荡主要依赖于短波辐射的日变化 ,短波辐射是SST的主要维持机制 ;短波辐射会使SST升高 1— 4℃ ;风的垂直混合作用主要是抑制了SST的日周期振荡。春季南海海面潜热通量和感热通量与短波辐射和风应力相比较 ,是一个对SST影响较小的量。南海北部 5月份混合层深度的变化趋势和振荡特征受风应力和短波辐射共同控制 ,风应力使混合层深度加深 5— 1 0m ,短波辐射使混合层深度平均变浅 5— 1 0m。而 6月份南海北部 ,在夏季风爆发后短波辐射较小 ,短波辐射的作用只能使混合层深度变浅1— 2m ,潜热通量和感热通量对混合层的作用会使混合层的深度加深 1— 2m ,混合层深度主要受风应力控制。

 
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