River-discharge effects on United States Atlantic and Gulf coast sea-level changes

• Published in: Proceedings of the National Academy of Sciences - PNAS 2018-07, Vol.115 (30), p.7729-7734
• Main Authors: Piecuch, Christopher G., Bittermann, Klaus, Kemp, Andrew C., Ponte, Rui M., Little, Christopher M., Engelhart, Simon E., Lentz, Steven J.
• Format: Article
• Language: English
• Subjects: Climate models; Coastal environments; Density stratification; Earth rotation; Environmental risk; Floods; Land ice; Ocean circulation; Ocean currents; Ocean dynamics; Physical oceanography; Physical Sciences; Population density; Remote sensing; River discharge; River flow; Rivers; Sea level changes; Sea level rise; Stream flow; Water circulation; Water discharge; Water storage
• ISSN: 0027-8424; 1091-6490
• DOI: 10.1073/pnas.1805428115

Identifying physical processes responsible for historical coastal sea-level changes is important for anticipating future impacts. Recent studies sought to understand the drivers of interannual to multidecadal sea-level changes on the United States Atlantic and Gulf coasts. Ocean dynamics, terrestrial water storage, vertical land motion, and melting of land ice were highlighted as important mechanisms of sea-level change along this densely populated coast on these time scales. While known to exert an important control on coastal ocean circulation, variable river discharge has been absent from recent discussions of drivers of sea-level change. We update calculations from the 1970s, comparing annual river-discharge and coastal sea-level data along the Gulf of Maine, Mid-Atlantic Bight, South Atlantic Bight, and Gulf of Mexico during 1910–2017. We show that river-discharge and sea-level changes are significantly correlated (p < 0.01), such that sea level rises between 0.01 and 0.08 cm for a 1 km³ annual river-discharge increase, depending on region. We formulate a theory that describes the relation between river-discharge and halosteric sea-level changes (i.e., changes in sea level related to salinity) as a function of river discharge, Earth’s rotation, and density stratification. This theory correctly predicts the order of observed increment sea-level change per unit river-discharge anomaly, suggesting a causal relation. Our results have implications for remote sensing, climate modeling, interpreting Common Era proxy sea-level reconstructions, and projecting coastal flood risk.