Abstract
The wind stress is considered to consist of momentum flux to aqueous flows and direct transfer to long waves. At various wind velocities, compositions of the wind stress and spectral contributions of wave components to each portion are presented. The rôle of the Charnock expression is further clarified, and all previous proposals relating roughness elements to waves are critically reviewed.
DOI: https://doi.org/10.3402/tellusa.v38i2.11711 | Journal eISSN: 3035-9554
Language: English
Page range: 178 - 188
Submitted on: Mar 12, 1985
Accepted on: Aug 7, 1985
Published on: Jan 1, 1986
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1986 Jin Wu, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
