Interactions Between Nonlinear Internal Ocean Waves and the Atmosphere

Abstract The heterogeneity in surface roughness caused by transient, nonlinear internal ocean waves is readily observed in coastal waters. However, the quantifiable impact this heterogeneity has on the marine atmospheric surface layer has not been documented. A comprehensive data set collected from...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: David G. Ortiz‐Suslow, Qing Wang, John Kalogiros, Ryan Yamaguchi, Tony dePaolo, Eric Terrill, R. Kipp Shearman, Pat Welch, Ivan Savelyev
Format: Article
Language:English
Published: Wiley 2019-08-01
Subjects:
Online Access:https://doi.org/10.1029/2019GL083374
Description
Summary:Abstract The heterogeneity in surface roughness caused by transient, nonlinear internal ocean waves is readily observed in coastal waters. However, the quantifiable impact this heterogeneity has on the marine atmospheric surface layer has not been documented. A comprehensive data set collected from a unique ocean platform provided a novel opportunity to investigate the interaction between this internal ocean process and the atmosphere. Relative to the background atmospheric flow, the presence of internal waves drove wind velocity and stress variance. Furthermore, it is shown that the wind gradient adjusts across individual wave fronts, setting up localized shear that enhanced the air‐sea momentum flux over the internal wave packet. This process was largely mechanical, though secondary impacts on the bulk humidity variance and gradient were observed. This study provides the first quantitative analysis of this phenomenon and provides insights into submesoscale air‐sea interactions over a transient, internal ocean feature.
ISSN:0094-8276
1944-8007