Variability in Ocean Bottom Pressure Dynamics

Summary

Variations in ocean bottom pressure (OBP) reflect changes in the mass of overlying water and are a key diagnostic of ocean circulation, sea-level budgets and climate variability. These fluctuations arise from wind-driven transports, density redistribution, tides and mesoscale eddy activity, and they span timescales from days to decades. Satellite gravimetry missions such as GRACE and its follow-on (GRACE-FO) have revolutionised global OBP monitoring, while arrays of seafloor pressure gauges and inverted echo sounders provide essential ground truth. Analyses of empirical orthogonal functions reveal coherent basin-scale modes linked to atmospheric patterns such as the Southern Annular Mode, El Niño–Southern Oscillation and Pacific Decadal Oscillation. Seasonal cycles are dominated by wind-induced Ekman convergence and divergence, whereas interannual to decadal variations often track large-scale climate indices. High-resolution ocean models capture the broad features of OBP variability but can underperform in eddy-rich regions, highlighting the need for finer spatial resolution. Understanding OBP dynamics is crucial for quantifying global mean sea-level change, calibrating ocean models and improving forecasts of climate impacts on ocean mass redistribution.

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Variability in Ocean Bottom Pressure Dynamics publication trend

The graph below shows the total number of articles in variability in ocean bottom pressure dynamics across all publications each year (not limited to Nature Index journals).

Technical terms

Ocean bottom pressure (OBP): The force per unit area exerted by the column of water above a point on the seafloor, sensitive to changes in ocean mass.

GRACE-FO: A satellite mission that measures time-variable gravity to infer mass redistribution, including OBP variations.

Mascon: A mass concentration solution dividing Earth’s surface into discrete blocks for gravity inversion, used to derive OBP anomalies.

Pressure-recording inverted echo sounder (PIES): A seafloor instrument that measures bottom pressure and acoustic travel time to characterise water column properties.

References

  1. Validation and Evaluation of GRACE-FO Estimates with In Situ Bottom Pressure Array Measurements in the South China Sea. Remote Sensing (2023).
  2. Uncertainties of monthly ocean bottom pressure from Gravity Recovery and Climate Experiment (GRACE): a case study at the Drake Passage. Geoscience Letters (2023).
  3. Ocean Bottom Pressure Variability: Can It Be Reliably Modeled?. Journal of Geophysical Research - Oceans (2020).
  4. On the seasonal variations of ocean bottom pressure in the world oceans. Geoscience Letters (2021).
  5. The Global Patterns of Interannual and Intraseasonal Mass Variations in the Oceans from GRACE and GRACE Follow-On Records. Remote Sensing (2022).

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