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Gough, M.K. (author), Reniers, A.J.H.M. (author), MacMahan, JH (author), Howden, SD (author)
The inertial frequency is nearly diurnal at 30°N latitude which transects the northeastern Gulf of Mexico (NeGoM). At this latitude, near-surface inertial oscillations can amplify due to resonance with diurnal wind forcing. Diurnal oscillations have also been attributed to diurnal tidal forcing in this region. Because tidal forcing, wind forcing...
journal article 2016
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Mariano, A.J. (author), Ryan, E.H. (author), Huntley, H.S. (author), Laurindo, L.C. (author), Coelho, E. (author), Ozgokmen, TM (author), Berta, M. (author), Bogucki, D (author), Chen, S.S. (author), Curcic, M. (author), Drouin, K.L. (author), Gough, M (author), Haus, BK (author), Haza, A.C. (author), Hogan, P (author), Iskandarani, M (author), Jacobs, G (author), Kirwan Jr., A.D. (author), Laxague, N (author), Lipphardt Jr., B. (author), Magaldi, M.G. (author), Novelli, G. (author), Reniers, A.J.H.M. (author), Restrepo, J.M. (author), Smith, C (author), Valle-Levinson, A. (author), Wei, M. (author)
The Grand LAgrangian Deployment (GLAD) used multiscale sampling and GPS technology to observe time series of drifter positions with initial drifter separation of O(100 m) to O(10 km), and nominal 5 min sampling, during the summer and fall of 2012 in the northern Gulf of Mexico. Histograms of the velocity field and its statistical parameters are...
journal article 2016