Mapping and Wavenumber Resolution of Line-Integral Data for Observations of Low-Mode Internal Tides

Techniques are developed for using line-integral tomography data to estimate the spectra, maps, and energy of low-mode internal-tide radiation; the extension of these techniques to other phenomena is obvious. Sparse arrays of line integrals over paths 300–1000 km long can generally determine the direction of propagation of semidiurnal radiation well, but the magnitude of the wavenumbers is ambiguous because of sidelobes in the spectrum. Both wavenumber magnitude and direction can generally be determined for diurnal internal-tide radiation. Spectra for the semidiurnal and diurnal internal tides are estimated for the region of the Atlantic Ocean between Puerto Rico and Bermuda using data obtained during the Acoustic Mid-Ocean Dynamics Experiment (AMODE) in 1991–92. Simulations of semidiurnal internal-tide radiation, consisting of wave packets or highly irregular wave crests, are used to show that the line-integral data provide better mapping resolution than point data, but the best results are, of ...