Dynamics of satellite‐derived interannual ocean bottom pressure variability in the western tropical North Pacific

Ocean bottom pressure variability, derived from Release‐05 Gravity Recovery and Climate Experiment time‐variable gravity coefficients over the ocean, is investigated along the tropical North Pacific for the case of long time scales (>1 yr) and large space scales (>750 km). To interpret the observations, a linear model of the bottom pressure response to interior wind stress curl is derived on the basis of normal vertical modes; the adjustment comprises contributions from barotropic Sverdrup dynamics as well as first baroclinic mode Rossby waves. Model solutions are evaluated numerically using time‐mean ocean stratification from the Ocean Comprehensible Atlas and time‐varying surface wind stress from the European Centre for Medium‐Range Weather Forecasts ERA‐Interim reanalysis. In the western tropical North Pacific, model and data compare favorably; simulated and observed time series are significantly correlated, and the model generally explains more than half of the data variance; the good correspondence between model and data speaks to the good quality of the satellite‐derived fields. In the central and eastern tropical North Pacific, findings are more ambiguous; model and data time series are mostly not significantly correlated, and simulations generally explain less than half of the data variance; discrepancies between model and data could point to physics absent from the model, for example, signals generated at the eastern boundary. Results provide observational demonstration that baroclinic contributions to bottom pressure changes can be important at low latitudes and low frequencies; findings hint at a basin‐scale influence of tropical climate modes on the ocean bottom pressure field.