Similarity And Dissimilarity In Air–seaMomentum And CO2 Transfers: TheNondimensional Transfer Coefficients In Light OfThe Windsea Reynolds Number
Similarity And Dissimilarity In Air–seaMomentum And CO2 Transfers: TheNondimensional Transfer Coefficients In Light OfThe Windsea Reynolds Number
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海气动量与二氧化碳传递的异同：风海雷诺数的无量纲传递系数
DOI：
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发表时间：
2006
期刊：
影响因子：
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通讯作者：
D. Zhao
中科院分区：
文献类型：
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作者：
Y. Toba;S. Komori;Yasushi Suzuki;D. Zhao
从量纲考虑，推导出在风-风-海平衡中，流体动力学条件仅可用两个无量纲参数来描述。一是代表性风浪的波龄。这描述了相对于当地风的风海发展程度。另一个是风浪雷诺数RB，定义为u2/νσp，其中u2是空气摩擦速度，ν是空气运动粘度，σp是风浪谱峰处的角频率。RB是由Toba和古贺于1986年提出的，以前它被表示为破碎波参数。它是风-海边界层的基本控制参数，因此也是海-气传输行为的基本控制参数。在研究传递系数的特性时，RB比10米风速、U 10或u 10的传递系数有上级的优势。传统上，海气CO2传输用传输速度kLas表示，kLas是U10的函数。我们建议使用无量纲转移
From dimensional considerations it is deduced that in wind–windsea equilibrium the fluid dynamical conditions can be described by only two nondimensional parameters. One is the wave age for the representative windsea. This describes the degree of windsea development relative to the local wind. The other is the windsea Reynolds number RB, which is defined by u 2 /νσp, where u∗ is the air friction velocity, ν is the air kinematic viscosity, and σp is the angular frequency at the windsea spectral peak. RBwas introduced by Toba and Koga in 1986, and formerly it was denoted as the breaking-wave parameter. It is the fundamental controlling parameter for the windsea boundary layer, and consequently for the behavior of air–sea transfers. RBis shown to be much superior to the 10-m wind speed, U10 or u∗, in studying the behavior of transfer coefficients. The air–sea CO2 transfer has traditionally been expressed in terms of a transfer velocity kLas a function of U10. We propose the use of a nondimensional transfer