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.
夜间绿洲上整晚维持蒸发，并有负感热通量。
Evaporation can last in the whole night and there is negative sensible heat flux over oasis.
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.
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.
城市峡谷是城市感热通量的主要来源，因此，在研究城市气象时不能忽略城市峡谷的影响。
Urban canyon is the main source of urban sensible heat flux. Thus, urban canyon can not be neglected in the urban weather research.
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.
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.
试验分析结果表明：感热通量对观测要素的观测误差比较敏感，因而其计算结果的误差较大；
The results show: sensible heat flux are sensitive to observation error, so the error of model calculation is great;
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.
根据边界层高度和感热通量的关系，可知感热通量约占地面接收到的太阳直接辐射的30 % 。
According to the relation of the height of atmosphric boundary layer and sensible flux , it is attained that the sensible flux is about 30% of the solar radiation received by the ground.
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.
海洋热通量是海岸锋形成的关键因子， 其中感热通量使海陆温差加大是形成海岸锋锋生的重要条件。
The sensible and latent heat fluxes from the ocean are the key factors for the formation of coastal front, especially, the sensible heat flux is more important to the coastal frontogenesis.
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.
对计算结果的对比分析表明，用感热通量的非局地多尺度湍流计算方法能计算出感热通量的逆梯度输送，也能计算出青藏高原近中性层结条件下明显的感热通量。
Analysis of the calculations shows that the first method is responsible for the upgradient transport of sensible heat and for the higher fluxes in the near-neutral stratification over the Plateau.
这表明森林通过降低地表反射率和表面温度，不仅增加地表净辐射，而且减少其用于感热和土壤热通量的消耗。
It is showed that the forest can not only increase net radiation but also decrease sensible and soil heat fluxes by decreasing surface reflectance and temperature.
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.
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.
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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