Procedures of formal averaging over the air-sea interface are applied to both momentum and enthalpy surface-transfer coefficients, C_D and C_K, in hurricane conditions. The transfer coefficients across the total area of the sea surface and water-covered portions of the sea surface, C_D, C_K, and C_Dw, C_Kw, are estimated by measurements in the open-sea and laboratory (foam-free) conditions, respectively, while the transfer coefficients across the foam-covered portion of the sea surface, C_{Df, Kf}, which cannot be measured directly, are estimated using the splitting relations. Applying the Monin-Obukhov similarity theory at the neutral stability atmospheric conditions to the transfer coefficients (separately for the foam-free, foam-covered, and total sea surfaces) yields the roughness lengths Z_Dw, Z_Kw, Z_Df, Z_Kf, and Z_D, Z_K. The study is aimed at the description of an anomalous, as compared with laboratory conditions, behavior of the momentum and enthalpy transfer coefficients in hurricane conditions with wind speed U₁₀ by the effect of the foam slipping layer sandwiched between the atmosphere and the ocean.

中文翻译：

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飓风中穿过泡沫覆盖的海气界面的动量和热传递

在飓风条件下，对海气界面进行形式平均的程序适用于动量和焓的表面传递系数C _D和C _K。通过在公海和实验室（无泡沫）的测量值估算出海面总面积和海面积水部分的传递系数C _D，C _K和C _Dw，C _Kw。条件，而跨海表层泡沫覆盖部分的传递系数C _Df，Kf不能直接测量的，使用分裂关系进行估算。将莫宁-奥布霍夫相似性理论在中性稳定大气条件下应用于传递系数（分别针对无泡沫，覆有泡沫和总海面使用）得出粗糙度长度Z _Dw，  Z _Kw，Z _Df，  Z _Kf，和ž _d，ž _ķ。该研究旨在描述与实验室条件相比异常的情况，在风速为U _10的飓风条件下，动量和焓传递系数的行为 通过夹在大气和海洋之间的泡沫滑脱层的作用。