地表潜热通量（Surface Latent Heat Flux，SLHF）反映了地表系统与大气之间的水热交换，它主要 是由于水的相变（凝结、蒸发、融化）所吸收或释放的热量。
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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.
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。
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.
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。
Three additional sensitive experiments are carried out to investigate the effect of condensation latent heating, evaporation cooling and surface heat flux.
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。
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