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%;
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