1National Oceanography Centre, Joseph Proudman Building, 6 Brownlow St, Liverpool L3 5DA, UK
2School of Environmental Sciences, University of Liverpool, Liverpool L69 3GP, UK
Received: 10 Oct 2013 – Discussion started: 05 Feb 2014
Abstract. We use ocean bottom-pressure measurements from 17 tropical sites to determine the annual cycle of ocean mass. We show that such a calculation is robust, and use three methods to estimate errors in the mass determination. Our final best estimate, using data from the best sites and two ocean models, is that the annual cycle has an amplitude of 0.85 mbar (equivalent to 8.4 mm of sea level, or 3100 Gt of water), with a 95% chance of lying within the range 0.61–1.17 mbar. The time of the peak in ocean mass is 10 October, with 95% chance of occurring between 21 September and 25 October. The simultaneous fitting of annual ocean mass also improves the fitting of bottom-pressure instrument drift.
Revised: 27 Jun 2014 – Accepted: 02 Jul 2014 – Published: 11 Aug 2014
Williams, J., Hughes, C. W., Tamisiea, M. E., and Williams, S. D. P.: Weighing the ocean with bottom-pressure sensors: robustness of the ocean mass annual cycle estimate, Ocean Sci., 10, 701-718, doi:10.5194/os-10-701-2014, 2014.