随水层深度的增加，水温日振幅逐渐减小，位相滞后也愈加明显。
Daily amplitude of water temperature gradually decreased and phase lagged more obviously with the increase of water depth.
对于土质均匀的砂质土壤，其土壤热通量日变化振幅最大，土壤的垂直热量交换最剧烈。
For homogeneous sandy loam soil, the diurnal variation amplitude of soil heat flux is very large, indicating the vertical heat exchanged is very strong.
模拟的SST日变化振幅水平分布与观测接近，且受太阳辐射日变化振幅水平分布调制。
The horizontal distribution of diurnal amplitude of simulated SST is consistent with that of observed SST and modulated by diurnal amplitude of solar radiation.
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