Using ECCO Estimates for Studies in Geodesy

Standard deviations of noise (thick bars) and signals (thin bars) for mass, velocity, and total OAM. ECCOv4 (red), ECCO-JPL (black) and GFZ (blue); Χ1, Χ2, and Χ3 from top to bottom.

Standard deviations of noise (thick bars) and signals (thin bars) for mass, velocity, and total OAM. ECCOv4 (red), ECCO-JPL (black) and GFZ (blue); Χ1, Χ2, and Χ3 from top to bottom.
References
Quinn, K.J., Ponte, R.M, Heimbach, P., Fukumori, I., and Campin, J.-M., (2018). Ocean Angular Momentum from a Recent Global State Estimate, with Assessment of Uncertainties, Geophys. J. Int., 216(1), 584-597, doi: 10.1093/gji/ggy452.Davis, J. and Vinogradova, N. (2017). Causes of Accelerating Sea Level on the East Coast of North America, Geophys. Res. Lett., 44, doi: 10.1002/2017GL072845.
van Dam, T., Collilieux, X., Wuite, J., Altamimi, Z., and Ray, J. (2012). Nontidal Ocean Loading: Amplitudes and Potential Effects in GPS Height Time Series, J. Geod., 86, 1043-1057, doi: 10.1007/s00190-012-0564-5.
Volkov, D.L. and Zlotnicki, V. (2012). Performance of GOCE and GRACE-derived Mean Dynamic Topographies in Resolving Antarctic Circumpolar Current Fronts, Ocean Dyn., 62, 893-905, doi: 10.1007/s10236-012-0541-9.
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