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Sean Haney, Baylor Fox-Kemper, Keith Julien, and Adrean Webb

in the advection of momentum, but the Stokes drift itself is not advected. The Stokes shear force is the primary driver of Langmuir cell instabilities (LC; e.g., Craik 1977 ); however, here modifications to other baroclinic instabilities by Stokes drift are of the greatest interest. None of the instabilities mentioned above, or the finite-amplitude features that they grow into, are resolved in global climate models (GCMs). With the finest-scale GCM simulations at ≈0.1° (≈10 km) resolution, even

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