Spatio-temporal variability of internal waves in the northern Gulf of Mexico studied with the Navy Coastal Ocean Model, NCOM

Mustafa Kemal Cambazoglu1, Gregg A. Jacobs2, Stephan Dixon Howden3, Jeffrey W Book4, Robert Arnone1, Inia M Soto Ramos5, Ryan Anthony Vandermeulen6, Adam T Greer5 and Travis N Miles7, (1)The University of Southern Mississippi, Division of Marine Science, Stennis Space Center, MS, United States, (2)Naval Research Lab, Stennis Space Center, MS, United States, (3)University of Southern Mississippi, Stennis Space Center, MS, United States, (4)U.S. Naval Research Laboratory, Stennis Space Center, MS, United States, (5)University of Southern Mississippi, Department of Marine Science, Stennis Space Center, MS, United States, (6)NASA Goddard Space Flight Center/SSAI, Ocean Ecology Laboratory, Greenbelt, MD, United States, (7)Rutgers University, Marine and Coastal Sciences, New Brunswick, NJ, United States
Abstract:
Internal waves enhance mixing in the upper ocean, transport nutrients and plankton over the water column and across the shelf from deeper waters to shallower coastal areas, and could also transport pollutants such as hydrocarbons onshore during an oil spill event. This study aims to characterize internal waves in the northern Gulf of Mexico (nGoM) and investigate the possible generation and dissipation mechanisms using a high-resolution (1-km) application of the Navy Coastal Ocean Model (NCOM). Three dimensional model products are used to detect the propagation patterns of internal waves. The vertical structure of internal waves is studied and the role of stratification is analyzed by looking at the temperature, salinity and velocity variations along the water column. The model predictions suggest the generation of internal waves on the continental shelf, therefore the role of ocean bottom topography interacting with tides and general circulation features such as the Loop Current Eddy front, on the internal wave generation will be discussed. The time periods of internal wave occurrences are identified from model predictions and compared to satellite ocean color imagery. Further data analysis, e.g. Fourier analysis, is implemented to determine internal wavelengths and frequencies and to determine if the response of internal waves are at tidal periods or at different frequencies. The atmospheric forcing provided to NCOM and meteorological data records are analyzed to define the interaction between wind forcing and internal wave generation. Wavelet analysis characterizes the ocean response to atmospheric events with periodic frequencies. Ocean color satellite imagery was used to visualize the location of the Mississippi river plume (and other oceanic features) and compared to the model predictions because the enhanced stratification from freshwater plumes which propagate across the Mississippi Bight can provide favorable conditions in coastal waters for internal wave generation and propagation. The findings of this study will provide insight about the internal wave dynamics in the Gulf of Mexico and their potential impact on the marine ecosystem.