latent heat net flux

基本解釋

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.
在黃土高原半乾旱地區(qū)：白天，潛熱通量在淨輻射通量的分配中所佔的份額最大，其次爲感熱通量，土壤熱通量最小。
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.
以微氣候觀測爲基礎，研究晴天狀況下海北高寒草甸地區(qū)淨輻射通量、土壤熱通量、感熱通量和潛熱通量變化等特征。
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.
通過反縯地表反照率、地表溫度、地表比輻射系數(shù)等蓡數(shù)，進一步計算出地表淨輻射通量、土壤熱通量、顯熱通量，根據(jù)地表能量平衡方程進行了蒸散的遙感反縯；