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根据１９９４年９月１８～３０日南沙群岛海域渚碧礁的近海面大气湍流观测实验资料，分别计算了该海域光滑海面和粗糙海面上的空气动力粗糙度（ｚ０ ）、中性曳力系数（ Ｃ Ｄ Ｎ）。利用 Ｂｕｔｓａｅｒｔ 的假定，推导了求取标量粗糙度（ｚ Ｔ、ｚ Ｑ）、整体输送系数（感热交换系数 Ｃ Ｈ Ｎ、水汽交换系数 Ｃ Ｅ Ｎ ）的一组公式。在此基础上，分别计算和分析了该海域光滑海面和粗糙海面上空气动力粗糙度（ｚ０ ）、标量粗糙度（ｚ Ｔ、ｚ Ｑ ）、中性曳力系数（ Ｃ Ｄ Ｎ）、整体输送系数（感热交换系数 Ｃ Ｈ Ｎ、水汽交换系数 Ｃ Ｅ Ｎ）及其关于水平风速分量的分布，并得到了一些有益的结论。
According to the observation data of near-surface atmospheric turbulence in Zhubi Reef, Nansha Islands waters from 18 to 30 September 1994, the aerodynamic roughness (z0), the neutral drag coefficient C D N). Based on Butsaert’s assumptions, a set of formulas for determining the scalar roughness (z T, z Q) and the overall transport coefficient (sensible heat exchange coefficient C H N, water vapor exchange coefficient C E N) are derived. On this basis, the aerodynamic roughness (z0), scalar roughness (z T, z Q), neutral drag coefficient (C D N), the overall transport Coefficient (sensible heat exchange coefficient C H N, water vapor exchange coefficient C E N) and its distribution about horizontal wind speed components, and some useful conclusions are obtained.