There was a consistency of the sensible and latent heat fluxes estimating by Profile gradient method, Bowen ratio energy balance method and Eddy covariance method (EC). Application of these methods to estimate wetland water heat flux was feasible.
生长季,廓线法模拟的水热通量更接近于观测值;但非生长季,波文比能量平衡法模拟的水热通量更接近于观测值。
参考来源 - 盘锦芦苇湿地碳通量特征与模拟研究·2,447,543篇论文数据,部分数据来源于NoteExpress
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