Feedback of tropical instability wave induced atmospheric variability onto the ocean

The effects of atmospheric feedbacks on tropical instability waves (TIWs) in the equatorial Atlantic Ocean are examined using a regional high-resolution coupled climate model. The analysis from a 6-yr hindcast from 1999 to 2004 reveals a negative correlation between TIW-induced wind perturbations and TIW-induced ocean currents, which implies damping of the TIWs. On the other hand, the feedback effect from the modification of Ekman pumping velocity by TIWs is small compared to the contribution to TIW growth by baroclinic instability. Overall, the atmosphere reduces the growth of TIWs by adjusting its wind response to the evolving TIWs. The analysis also shows that including ocean current (mean + TIWs) in the wind stress parameterization reduces the surface stress estimate by 15%-20% over the region of the South Equatorial Current. Moreover, TIW-induced perturbation ocean currents can significantly alter surface stress estimations from scatterometers, especially at TIW frequencies. Finally, the rectification effect from the atmospheric response to TIWs on latent heat flux is small compared to the mean latent heat flux.

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Author Seo, Hyodae
Jochum, Markus
Murtugudde, Maghu
Miller, Arthur
Roads, John
Publisher UCAR/NCAR - Library
Publication Date 2007-12-01T00:00:00
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Topic Category geoscientificInformation
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Metadata Date 2023-08-18T18:26:57.511851
Metadata Record Identifier edu.ucar.opensky::articles:6951
Metadata Language eng; USA
Suggested Citation Seo, Hyodae, Jochum, Markus, Murtugudde, Maghu, Miller, Arthur, Roads, John. (2007). Feedback of tropical instability wave induced atmospheric variability onto the ocean. UCAR/NCAR - Library. http://n2t.net/ark:/85065/d78g8kz2. Accessed 15 March 2025.

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