Stochastic Stability of Open-Ocean Deep Convection
- 1 December 2003
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 33 (12) , 2764-2780
- https://doi.org/10.1175/1520-0485(2003)033<2764:ssoodc>2.0.co;2
Abstract
Open-ocean deep convection is a highly variable and strongly nonlinear process that plays an essential role in the global ocean circulation. A new view of its stability is presented here, in which variability, as parameterized by stochastic forcing, is central. The use of an idealized deep convection box model allows analytical solutions and straightforward conceptual understanding while retaining the main features of deep convection dynamics. In contrast to the generally abrupt stability changes in deterministic systems, measures of stochastic stability change smoothly in response to varying forcing parameters. These stochastic stability measures depend chiefly on the residence times of the system in different regions of phase space, which need not contain a stable steady state in the deterministic sense. Deep convection can occur frequently even for parameter ranges in which it is deterministically unstable; this effect is denoted wandering unimodality. The stochastic stability concepts are rea... Abstract Open-ocean deep convection is a highly variable and strongly nonlinear process that plays an essential role in the global ocean circulation. A new view of its stability is presented here, in which variability, as parameterized by stochastic forcing, is central. The use of an idealized deep convection box model allows analytical solutions and straightforward conceptual understanding while retaining the main features of deep convection dynamics. In contrast to the generally abrupt stability changes in deterministic systems, measures of stochastic stability change smoothly in response to varying forcing parameters. These stochastic stability measures depend chiefly on the residence times of the system in different regions of phase space, which need not contain a stable steady state in the deterministic sense. Deep convection can occur frequently even for parameter ranges in which it is deterministically unstable; this effect is denoted wandering unimodality. The stochastic stability concepts are rea...Keywords
This publication has 39 references indexed in Scilit:
- Potential causes of abrupt climate events: A numerical study with a three‐dimensional climate modelGeophysical Research Letters, 2002
- An abrupt climate event in a coupled ocean–atmosphere simulation without external forcingNature, 2001
- Improved estimates of global ocean circulation, heat transport and mixing from hydrographic dataNature, 2000
- Intermittent convection, mixed boundary conditions and the stability of the thermohaline circulationClimate Dynamics, 1999
- Signature of recent climate change in frequencies of natural atmospheric circulation regimesNature, 1999
- Convective Adjustment and Thermohaline ExcitabilityJournal of Physical Oceanography, 1996
- Long-term coordinated changes in the convective activity of the North AtlanticProgress in Oceanography, 1996
- A Simple Box Model of Stochastically Forced Thermohaline FlowJournal of Physical Oceanography, 1994
- The “great salinity anomaly” in the Northern North Atlantic 1968–1982Progress in Oceanography, 1988
- Stochastic climate models Part I. TheoryTellus, 1976