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本文提出仅需若干特定层次的风速与气温的观测(或计算)值便可算出大气稳定度的5个简化式。计算结果显示:(1)所论海区可沿用风速的对数律,而(气温—表面水温)的对数律是有条件地被采用;(2)R_1=R_2,R_1=ζ_2和ζ_3=ζ_2。
In this paper, we propose five simplified formulas that can be used to calculate the atmospheric stability by only observing (or calculating) the values of wind speed and temperature at some specific levels. The results show that: (1) logarithmic law of wind speed can be used in the sea area concerned, and logarithm law of (air temperature - surface water temperature) is adopted conditionally; (2) R_1 = R_2, R_1 = ζ_2 and ζ_3 = ζ_2 .