A Simple Model of the Response of the Atlantic to the North Atlantic Oscillation
Journal of Climate American Meteorological Society 27:11 (2014) 4052-4069
Advection of baroclinic eddies by depth mean flow
Geophysical Research Letters American Geophysical Union (AGU) 41:10 (2014) 3517-3521
What methotrexate side effects are rheumatology patients living with?
SCOTTISH MEDICAL JOURNAL 59:4 (2014) E39-E39
Rossby rip currents
Geophysical Research Letters 40:16 (2013) 4333-4337
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.Conceptual models of the wind-driven and thermohaline circulation
103 (2013) 257-282