David Marshall

Abstract:

2013 U.S. AMOC–U.K. RAPID INTERNATIONAL SCIENCE MEETING

What: A total of 106 U.S. and international participants, including academic and governmental climate scientists and funding agency managers, met to review current research findings using paleo- and modern observational data, theory, modeling, and predictability/prediction experiments to explore the variability of the Atlantic meridional overturning circulation (AMOC) and its impacts on climate, sea level, carbon/biogeochemistry, and ecosystems.

When: 16–19 July 2013

Where: Baltimore, Maryland

Abstract:

Oceanic Rossby waves and eddies flux energy and fluid westward, the latter through the Stokes drift or bolus transport. While the wave energy is largely dissipated at the western boundary, mass conservation requires that the fluid be returned offshore through Rossby rip currents. The form and magnitude of these rip currents are investigated through linear Rossby wave theory, a nonlinear numerical model, and analysis of sea surface height satellite observations. The net eastward volume transport by Rossby rip currents over the global ocean is estimated to be of order 10 Sv (1 Sv ≡106 m3 s -1). In an eddying ocean, both the westward Stokes drift and eastward rip currents can assume the form of banded quasi-zonal jets. Key Points Oceanic Rossby waves and eddies carry a westward Stokes drift The westward Stokes drift may be compensated by eastward Rossby rip currents Both the Stokes drift and rip currents can assume the form of banded zonal jets. © 2013. American Geophysical Union. All Rights Reserved.