| Summary: | A netcdf data file of high-frequency (> 1 cpd) baroclinic mode-1 amplitude in the western North Atlantic derived from ocean acoustic tomography data collected during the Acoustic Mid-Ocean Dynamics Experiment (AMODE) in 1991. AMODE consisted of a pentagonal array of six moored instruments deployed between Puerto Rico and Bermuda. These are baroclinic amplitudes averaged over paths several hundred kilometers long. As documented in: Dushaw, B. D., & Worcester, P. F. (1998). Resonant diurnal internal tides in the North Atlantic. Geophys. Res. Lett., 25 , 2189–2192. doi:10.1029/98GL01583 Dushaw, B. D., Worcester, P. F., Cornuelle, B. D., Howe, B. M., & Luther, D. S. (1995). Baroclinic and barotropic tides in the central North Pacific Ocean determined from long-range reciprocal acoustic transmissions.J. Phys. Oceanogr.(25), 631–647. doi:10.1175/1520-0485(1995)025〈0631: BABTIT〉2.0.CO;2 Dushaw, B. D. (2003). On the mapping and wavenumber resolution of line-integral data for observations of low-mode internal tides. J. Atmos. Oceanic Tech., 20 , 1043–1059. doi:10.1175/1458.1 Dushaw, B. D. (2006). Mode-1 internal tides in the western North Atlantic Ocean. Deep-Sea Res. Part I , 53 , 449–473. doi:10.1016/j.dsr.2005.12.009 Dushaw, B. D., Worcester, P. F., & Dzieciuch, M. A. (2011). On the predictability of mode-1 internal tides. Deep-Sea Res. Part I (58), 677–698. doi:10.1016/j.dsr.2011.04.002 Dushaw, B. D. (2015). An empirical model for mode-1 internal tides derived from satellite altimetry: Computing accurate tidal predictions at arbitrary points over the world oceans (Tech. Rep. No. Technical Memorandum TM 1-15). Applied Physics Laboratory, University of Washington, Seattle, WA. http://www.apl.washington.edu/project/project.php?id=tm\ 1-15 Hendershott, M. (1981). Long waves and ocean tides. In B. A. Warren & C. Wunsch (Eds.), Evolution of physical oceanography: Scientific surveys in honor of Henry Stommel (pp. 292–341). Cambridge, MA: MIT Press. These data can be used to derive accurate estimate for ...
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