Tidal Geopotential Dependence on Earth Ellipticity and Seawater Density and Its Detection With the GRACE Follow‐On Laser Ranging Interferometer. Issue 12 (30th November 2020)

• Record Type: Journal Article
• Authors: Han, Shin‐Chan; Ghobadi‐Far, Khosro; Ray, Richard D.; Papanikolaou, Thomas
• Is Part Of: Journal of geophysical research. Volume 125:Issue 12(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-11-30
• Subjects: Ocean tide -- Time‐variable gravity -- GRACE -- GRACE Follow‐On -- ellipticity -- seawater density; Oceanography -- Periodicals; 551.4605
• DOI: 10.1029/2020JC016774
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract: Ocean tides produce significant gravitational perturbations that affect near‐Earth orbiting spacecraft. The gravitational potential induced by tidal mass redistribution is routinely modeled for global gravity analysis and orbit determination, although generally by assuming a spherical Earth and a uniform seawater density. The inadequacy of these simplifications is here addressed. We have developed an accurate yet efficient algorithm to compute the ocean tidal geopotential, allowing for Earth's elliptical shape and variable seawater density. Using this new computation, we find that (1) the effect of ellipticity is several percent of the tide signal over mid to high‐latitude regions, which is comparable to elevation error in the state‐of‐the‐art ocean tide models; (2) the effect of seawater density variations on the potential is as large as 2–3 cm in water‐height equivalent, primarily in deep water where density increases 2%–3% from compressibility. Our analysis of new Gravity Recovery and Climate Experiment Follow‐On (GRACE‐FO) laser ranging interferometer measurements reveals evident errors when ellipticity and density variations are ignored. When accounted for, the GRACE‐FO residual tidal gravity perturbations are reduced by half, depending on the adopted tide model; only the remaining half likely represents actual model elevation error. The use of a spherical surface and a uniform seawater density is no longer tenable given the precision of gravity measurements from GRACE and GRACE‐FO satellites. Plan Language Summary: Ocean tide involves periodic mass redistribution and changes global Earth gravity fields. The gravitational attraction by ocean tidal mass has been routinely modeled for analyzing Earth‐orbiting spacecraft data and computing Earth's gravity field changes. Generally, the spherical Earth and a uniform seawater density are assumed for mass change by ocean tide. The Earth ellipticity and seawater density variation have not yet been adequately discussed in the literature on time‐variable gravity and orbit analysis. We present new results from the analysis of actual Gravity Recovery and Climate Experiment Follow‐On (GRACE‐FO) laser ranging interferometer measurements and report that the use of spherical Earth and uniform seawater density is no longer tenable given the precision of gravity measurements from GRACE and GRACE‐FO satellites. We recommend the GRACE and GRACE‐FO processing centers to revise their computations of the ocean tide's gravitational potential using the algorithm and computer code in this study. Key Points: New algorithm to compute global geopotential from ocean tidal mass change considering the ellipticity and seawater density change The ellipticity and density effects (often neglected in orbit & gravity analysis) were found to be as large as tidal elevation model errors. New GRACE Follow‐On laser ranging interferometer data observed these systematic errors by the ellipticity and seawater density change.