并且潜热通量明显高于感热通量。
The latent heat flux is much bigger than the sensible heat flux.
文中集中分析了表面感热和潜热通量的时空分布特征。
Special attention is paid to the diagnosis of the temporal and spatial distributions of surface sensible and latent heat fluxes.
分析结果表明在赤道海域，潜热通量远远大于感热通量。
The results show that the latent heat flux is much greater than the radiate heat flux.
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。
Then the latent heat flux was calculated through energy balance equation and the daily evapotranspiration was estimated.
观测的潜热通量与模拟的潜热通量的相关系数达到0.97，高估13%。
The correlation coefficient of observed latent heat and simulated latent heat is 0.97 and SiB2 overestimates it 13%.
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。
The structure parameter of refractive index imaginary part for the different latent heat flux was calculated by means of simulation theory.
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。
The phenomenons of negative sensible heat flux, large latent heat flux even over the net radiation were observed in sunny afternoon in the oasis.
热量平衡的各分量中，潜热通量占净辐射的比值最大，湍流热通量和土壤热通量均较小。
Among all component values of heat balance, the latent heat flux occupies the highest proportion from net radiation, both turbulence heat flux and soil heat flux occupy lower.
内陆地区的地震前常产生热红外异常，而沿海地区的地震前则更容易出现潜热通量异常。
Satellite infrared anomalies are often found before inland earthquakes, and anomalous increase of surface heat latent flux is usually discovered before the earthquakes in coastal areas.
我国东部海域及其向中东太平洋的延伸部分为冬季潜热通量和感热通量年际变化的关键区。
The East China Sea and its extension to the mid-eastern Pacific are the key regions of interannual variability of air-sea turbulent heat fluxes over the North Pacific.
此外，在该海域内，确定海面热量平衡特性的两个最重要的因素应属潜热通量和太阳辐射通量。
Additionally, the latent heat flux and solar radiation flux should be two of the most important factors in determining the sea surface heat balance in this region.
在坨甸相间地区生态系统的热量平衡中，占比例大的是潜热通量，其次为感热通量和土壤热通量。
In the heat balance of ecological system in dune alternated with wetland area, the latent heat flux takes the most share, in the next place is sensible heat flux and soil heat flux.
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。
In contrast, latent heat flux and momentum flux is not so sensitive to observation error as sensible heat, and their calculated results is reliable.
降雨之后，芦苇湿地生态系统水热通量都有所增加，尤其是潜热通量增加显著，且峰值出现时间提前。
After rain, the value of water and heat fluxes in reed wetland ecosystem increased and the peak value appeared ahead of time.
在绿洲荒漠过渡区生态系统的热量平衡中，占比例最大的是潜热通量，其次为感热通量和土壤热通量。
The biggest proportion in the heat balance is the potential heat flux, followed by sensible heat flux and soil heat flux.
在黄土高原半干旱地区：白天，潜热通量在净辐射通量的分配中所占的份额最大，其次为感热通量，土壤热通量最小。
In loess plateau, at the daytime, the net radiation contributes mainly to the latent heat flux, the sensible heat flux is minor and the soil heat flux is least.
以微气候观测为基础，研究晴天状况下海北高寒草甸地区净辐射通量、土壤热通量、感热通量和潜热通量变化等特征。
Based on a microclimate observation, a study, on fine days, of the net radiation flux, soil heat flux, sensible heat flux, and latent heat flux on the alpine meadows of Haibei Area was conducted.
研究城市非均匀地表能量通量的特征，绘制地表显热及潜热通量的区域分布图，对构筑绿色宜居城市具有重要的意义。
So study the characteristic of the non-uniform surface energy flux in the urban amd draw the regional distribution map of the energy flux surface, have important meanings.
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。
The turbulent coefficient and turbulent flux was decreased and the latent heat flux was increased by irrigation and vice versa by straw mulching.
进行三组敏感性试验，研究凝结潜热释放，蒸发冷却与地表热通量对气旋结构与强度的影响。
Three additional sensitive experiments are carried out to investigate the effect of condensation latent heating, evaporation cooling and surface heat flux.
高原效应的综合影响方面：地形抬升对地面感热通量的影响较小，对凝结潜热的影响明显。
For the integrated effects, the raising of TP has little influence on the surface sensible heat flux, while it greatly affects condensation heating.
与潜热的湍流输送及海表面向上的长波辐射通量相比，感热的湍流输送量很小。
Comparing with the flux of turbulent exchange of latent heat and the flux of upward long-wave radiation the flux of sensible heat exchange is very small.
对比结果表明： （1）当模式低估净辐射0.2%时， 模式分别高估感热、潜热和土壤热通量4%、 13%和8%；
Results show that: (1) SiB2 overestimated sensible, latent, and soil heat fluxes by 4%, 13%, and 8% respectively when it underestimated net radiation by 0.2%;
对比结果表明： （1）当模式低估净辐射0.2%时， 模式分别高估感热、潜热和土壤热通量4%、 13%和8%；
Results show that: (1) SiB2 overestimated sensible, latent, and soil heat fluxes by 4%, 13%, and 8% respectively when it underestimated net radiation by 0.2%;
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