Barystatic and manometric sea level variations based on sea level budget

Barystatic and manometric sea level changes represent the mass component of sea level changes at global and regional scales, respectively. Barystatic sea level changes are estimated using the sea level budget (SLB) approach combining satellite altimetry with in-situ measurements of the seawater temperature and salinity.

This SLB approach is adapted from Barnoud et al., (2023; https://doi.org/10.5194/os-19-321-2023). Manometric sea level variations and their uncertainties are not provided for the SLB approach, due to the high uncertainties associated with the drift of the halosteric component (e.g., Bouih et al., 2025; https://doi.org/10.5194/egusphere-egu24-16813).

Data and resources

Additional information

Temporal extent1993-01-01 – 2023-06-30
Date (creation)2023-04-27
Date (publication)2023-08-22
Date (lastUpdate)2025-11-27
Statuscompleted
Update frequencyasNeeded
Metadata languagefr
LicenseLicence Ouverte
Source metadataISO 19115 XML
Last updated2026-11-04
Created2026-11-04
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