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Exploring steric sea level variability in the Eastern Tropical Atlantic Ocean: a three-decade study (1993-2022)
Franck Eitel Kemgang Ghomsi1,2,3, Bayoumy Mohamed4,5, Roshin P Raj6
1Deutsches Geodätisches Forschungsinstitut, Technische Universität München (DGFI-TUM), Munich, Germany. franckeitel@gmail.com.
Sea level rise in the Eastern Tropical Atlantic Ocean (ETAO) is 3.52 mm/year, matching the global average. Ocean mass, not steric changes, drives long-term trends, necessitating urgent adaptation strategies for coastal communities.
Area of Science:
- Oceanography
- Climate Science
- Geophysics
Background:
- Sea level rise (SLR) threatens coastal populations globally, with over 60 million people in Africa living below 10m above sea level.
- The Eastern Tropical Atlantic Ocean (ETAO) is particularly vulnerable to SLR impacts.
Purpose of the Study:
- To analyze spatio-temporal trends of sea level anomaly (SLA) and its components in the ETAO from 1993 to 2022.
- To identify the drivers of SLR in the region and their correlation with climate factors.
Main Methods:
- Analysis of satellite altimetry data for SLA trends (1993-2022).
- Utilized ARMORD3D dataset for steric component analysis (thermosteric, halosteric).
- Incorporated GRACE and GRACE-FO mission data for ocean mass changes (2002-2022).
Main Results:
- ETAO exhibits an SLA trend of 3.52 ± 0.47 mm/year, consistent with the global average.
- Ocean mass changes dominate long-term SLR trends, while steric variations influence interannual variability.
- Warming observed along the equatorial African coast and Gulf of Guinea (GoG), with freshening near Angola.
Conclusions:
- Ocean mass, not steric expansion, is the primary driver of long-term sea level rise in the ETAO.
- Regional climate patterns significantly influence sea level changes.
- Urgent mitigation and adaptation strategies are crucial for vulnerable ETAO coastal communities.
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