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1·The latent heat flux is much bigger than the sensible heat flux.

并且潜热通量明显高于感热通量。

2·The results show that the latent heat flux is much greater than the radiate heat flux.

分析结果表明在赤道海域，潜热通量远远大于感热通量。

3·The results show that the ratio of the latent heat flux to the sensible heat flux is 10. 14;

指出西大平洋暖池海区游热通量与显效通量之比为10.14：1；

4·The net radiation and contribution of latent heat flux tend to decrease due to increasingly grazing intensity.

随放牧强度的增加，净辐射或净有效能减少，而且潜热交换的贡献也相对减少。

5·Then the latent heat flux was calculated through energy balance equation and the daily evapotranspiration was estimated.

然后通过能量平衡方程得到潜热通量，并推算得到日蒸散量值。

6·The structure parameter of refractive index imaginary part for the different latent heat flux was calculated by means of simulation theory.

不同潜热通量时，折射率的结构常数在满足相似理论的条件下可以计算出来。

7·Analysis of boundary layer fluxes shows that the amount of latent heat flux leaded to differ the Khanun's horizontal and vertical structure.

边界层方案的差异也导致台风动力和热力结构在水平和垂直分布上都出现显著差异。

8·The phenomenons of negative sensible heat flux, large latent heat flux even over the net radiation were observed in sunny afternoon in the oasis.

晴天下午绿洲经常出现感热通量为负，潜热通量超过净辐射的现象平流/局地环流。

9·The turbulent coefficient and turbulent flux was decreased and the latent heat flux was increased by irrigation and vice versa by straw mulching.

灌溉能够降低近地面的湍流交换系数和湍流热通量，提高潜热通量，而秸秆覆盖的作用相反。秸秆覆盖具有增强灌溉水入渗能力的作用。

10·In contrast, latent heat flux and momentum flux is not so sensitive to observation error as sensible heat, and their calculated results is reliable.

相反，潜热通量和动量通量对观测要素的观测误差相对不太敏感，因此，它们的计算结果比较可靠。