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- W2014367444 abstract "Abstract Several simple numerical experiments are conducted, using both single- and double-hemisphere ocean basins under symmetric steady forcing to study de ocean's thermohaline circulation. It is shown that a stable steady state obtained under a restoring surface boundary condition on salinity becomes unstable upon a switch to a flux boundary condition. The polar halocline catastrope of F. Bryan occurs. It is shown that further integration of this collapsed state ultimately yields a steady, stable one-cell circulation with the approach being essentially chaotic but with significant energy at decadal period. The two-hemisphere ocean passes through many stages in which violent overturning occurs O(80 × 101 m3 a−1). These flushes occurs in both hemispheres and are of one-cell structure. The time period between them Bushes varies from seveal hundred to about one thousand years. A single 12-vertical-level hemispheric basin, spun up from an initial state of rest under mixed boundary conditions (restoring boun..." @default.
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- W2014367444 date "1991-09-01" @default.
- W2014367444 modified "2023-10-12" @default.
- W2014367444 title "The Role of Mixed Boundary Conditions in Numerical Models of the Ocean's Climate" @default.
- W2014367444 doi "https://doi.org/10.1175/1520-0485(1991)021<1470:trombc>2.0.co;2" @default.
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