latent heat flux

基本解释

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。
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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.
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。
Firstly, the remote sensing method based on surface energy balance equation which is a function of net radiance flux, soil heat flux, sensible heat flux and latent heat flux is used to retrieve ET.
通过反演地表反照率、地表温度、地表比辐射系数等参数，进一步计算出地表净辐射通量、土壤热通量、显热通量，根据地表能量平衡方程进行了蒸散的遥感反演；

Latent heat flux is highly variable with low values during the accumulation season and high values during the dry period.
UNESCO: Dublin Core

潜热通量
Now it is mainly based on the surface energy balance equation. Latent heat flux can be derived from inversing net radiance, soil heat and sensible heat flux.
遥感反演主要立足于地表热量平衡方程，通过反演方程中的净辐射、土壤热流量和显热通量，进而推算出潜热通量。
环境科学技术
潜热通量