Articles | Volume 14, issue 1
Earth Syst. Sci. Data, 14, 229–249, 2022
https://doi.org/10.5194/essd-14-229-2022
Earth Syst. Sci. Data, 14, 229–249, 2022
https://doi.org/10.5194/essd-14-229-2022

Data description paper 26 Jan 2022

Data description paper | 26 Jan 2022

Monitoring the ocean heat content change and the Earth energy imbalance from space altimetry and space gravimetry

Florence Marti et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on essd-2021-220', Anonymous Referee #1, 11 Aug 2021
    • AC1: 'Reply on RC1', Marti Florence, 22 Oct 2021
  • RC2: 'Comment on essd-2021-220', Anonymous Referee #2, 18 Aug 2021
    • AC2: 'Reply on RC2', Marti Florence, 22 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Marti Florence on behalf of the Authors (22 Oct 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (06 Nov 2021) by Giuseppe M.R. Manzella
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Short summary
The Earth energy imbalance at the top of the atmosphere due to the increase in greenhouse gases and aerosol concentrations is responsible for the accumulation of energy in the climate system. With its high thermal inertia, the ocean accumulates most of this energy excess in the form of heat. The estimation of the global ocean heat content through space geodetic observations allows monitoring of the energy imbalance with realistic uncertainties to better understand the Earth’s warming climate.