Measurements of the viscous tangential stress in the airflow above wind waves
The stress and drag at the surface of the ocean are crucial parameters for both short term forecasting and the modeling of long‐term global climate trends. However, the partition between viscous, turbulent, and wave stresses, and in particular the effects of airflow separation are not well understoo...
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Published in: | Geophysical research letters Vol. 34; no. 19; pp. L19603 - n/a |
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Main Authors: | , , |
Format: | Journal Article |
Language: | English |
Published: |
Washington, DC
American Geophysical Union
01-10-2007
Blackwell Publishing Ltd |
Subjects: | |
Online Access: | Get full text |
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Summary: | The stress and drag at the surface of the ocean are crucial parameters for both short term forecasting and the modeling of long‐term global climate trends. However, the partition between viscous, turbulent, and wave stresses, and in particular the effects of airflow separation are not well understood. We present direct measurements of the velocity in the airflow above wind‐generated waves. We observe intermittent separation of the viscous sublayer past the crest of the wind waves leading to dramatic along‐wave variability in the surface viscous tangential stress. These results hold for wind speeds that would normally be considered low to moderate. These viscous stress measurements in the airflow above the wavy surface, and within the separated region are, to the best of the authors' knowledge, the first of this kind. |
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Bibliography: | istex:0A3E3398D94011FD02947820FB6EC4926A5D8A8F ArticleID:2007GL031242 ark:/67375/WNG-DDQV9S3R-G ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2007GL031242 |