Global observations of open-ocean mode-1 M2 internal tides

TitleGlobal observations of open-ocean mode-1 M2 internal tides
Publication TypeJournal Article
Year of Publication2016
AuthorsZhao Z, Alford MH, Girton JB, Rainville L, Simmons HL
JournalJournal of Physical Oceanography
Volume46
Pagination1657-1684
Date Published2016/05
KeywordsCirculation/ Dynamics,Internal waves,Atm/Ocean Structure/ Phenomena,Tides,Observational techniques and algorithms,Altimetry,Satellite observations,Mathematical and statistical techniques,Numerical analysis/modeling,Applications,Field experiments
Abstract

AbstractA global map of open-ocean mode-1 M2 internal tides is constructed using sea surface height (SSH) measurements from multiple satellite altimeters during 1992–2012, representing a 20-yr coherent internal tide field. A two-dimensional plane wave fit method is employed to 1) suppress mesoscale contamination by extracting internal tides with both spatial and temporal coherence and 2) separately resolve multiple internal tidal waves. Global maps of amplitude, phase, energy, and flux of mode-1 M2 internal tides are presented. The M2 internal tides are mainly generated over topographic features, including continental slopes, midocean ridges, and seamounts. Internal tidal beams of 100–300 km width are observed to propagate hundreds to thousands of kilometers. Multiwave interference of some degree is widespread because of the M2 internal tide’s numerous generation sites and long-range propagation. The M2 internal tide propagates across the critical latitudes for parametric subharmonic instability (28.8°S/N) with little energy loss, consistent with the 2006 Internal Waves across the Pacific (IWAP) field measurements. In the eastern Pacific Ocean, the M2 internal tide loses significant energy in propagating across the equator; in contrast, little energy loss is observed in the equatorial zones of the Atlantic, Indian, and western Pacific Oceans. Global integration of the satellite observations yields a total energy of 36 PJ (1 PJ = 1015 J) for all the coherent mode-1 M2 internal tides. Finally, satellite observed M2 internal tides compare favorably with field mooring measurements and a global eddy-resolving numerical model.

DOI10.1175/JPO-D-15-0105.1
Student Publication: 
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