Incoherent signature of internal tides on sea level in idealized numerical simulations. Issue 5 (13th March 2015)

• Record Type: Journal Article
• Authors: Ponte, A. L.; Klein, P.
• Is Part Of: Geophysical research letters. Volume 42:Issue 5(2015:Mar.)
• Page Start: 1520
• Page End: 1526
• Publication Date: 2015-03-13
• Subjects: internal tide -- wide‐swath altimetry -- mesoscale turbulence -- incoherence; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2014GL062583
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: The nonpersistent phase relationship between internal tides and astronomical forcings, also known as incoherence, has been identified as a major question in the context of future wide‐swath satellite altimetry. This study addresses this issue using a novel set of numerical experiments where a plane wave/low‐mode internal tide propagates through a turbulent mesoscale eddy field. These experiments demonstrate the emergence of internal tide incoherence as the eddy turbulence is strengthened. In strongly turbulent situations, the internal tide signature on sea level forms complex interference patterns with large amplifications of the initial internal wave. These patterns evolve more rapidly than the signature of the turbulent eddy field on sea level. The implications of such idealized numerical simulations for wide‐swath altimetry are discussed. Key Points: Idealized numerical simulations bring new light on internal tide incoherence Internal tides become incoherent as they interact with a turbulent eddy field The incoherence is sensitive to the magnitude of the eddy turbulence