A model for Dansgaard-Oeschger events and millennial-scale abrupt climate change without external forcing

Abstract

We propose a conceptual model which generates abrupt climate changes akin to Dansgaard-Oeschger events. In the model these abrupt climate changes are not triggered by external perturbations but rather emerge in a dynamic self-consistent model through complex interactions of the ocean, the atmosphere and an intermittent process. The abrupt climate changes are caused in our model by intermittencies in the sea-ice cover. The ocean is represented by a Stommel two-box model, the atmosphere by a Lorenz-84 model and the sea-ice cover by a deterministic approximation of correlated additive and multiplicative noise (CAM) process. The key dynamical ingredients of the model are given by stochastic limits of deterministic multi-scale systems and recent results in deterministic homogenisation theory. The deterministic model reproduces statistical features of actual ice-core data such as non-Gaussian $\alpha$-stable behaviour. The proposed mechanism for abrupt millenial-scale climate change only relies on the existence of a quantity, which exhibits intermittent dynamics on an intermediate time scale. We consider as a particular mechanism intermittent sea-ice cover where the intermittency is generated by emergent atmospheric noise. However, other mechanisms such as freshwater influxes may also be formulated within the proposed framework.

References in corpus (4)

• Marcus versus Stratonovich for Systems with Jump Noise
• Stochastic Climate Theory
• On the detection of superdiffusive behaviour in time series
• Simulation of non-Lipschitz stochastic differential equations driven by $\alpha$-stable noise: a method based on deterministic homogenisation

Cited by in corpus (3)

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• Lévy-noise versus Gaussian-noise-induced Transitions in the Ghil-Sellers Energy Balance Model
• Limits to predictability of the asymptotic state of the Atlantic Meridional Overturning Circulation in a conceptual climate model