The shape of the main thermocline, revisited
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ID: 308592
2010
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Abstract
UsingtheMonteCarlomethodofstatisticalphysics,wecomputetheequilibriumstatisticalmechanics of the shallow water equations, considered as a reduced-gravity model of the ocean’s upper layer in a square ocean that spans the equator. The ensemble-averaged flow comprises a westward drift at low latitudes, associated with the poleward deepening of the main thermocline, and a more intense compensating eastward flow near the latitudes at which the layer depth vanishes. Inviscid numerical simulations with a model that exactly conserves mass, energy, and potential enstrophy support the theoretical prediction.
| Reference Key |
openalex_W2148854588
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|---|---|
| Authors | Rick Salmon |
| Journal | journal of marine research |
| Year | 2010 |
| DOI |
10.1357/002224010794657182
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| URL | |
| Keywords | Keywords not found |
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