潮差: change of tidedifference of tiderange of flood and ebbrange of the tiderange of tidesretardation of tidetidal differencetidal rangetidal variationtidalrangetide range
半潮差: amplitude of tidehalf range of tidetide amplitude
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Both the asynchronous effect of synchronous reduction method and the time shift effect of regression reduction method are discovered and more precise models for both above methods developed in this paper 研究还表明：平均海面的回归分析传递法和深度基准面的潮差比传递法均是最小二乘潮位拟合传递法的特殊形式。
