Millennial-scale stable oscillations between sea ice and convective deep water formation

TL;DR

This paper introduces a simple dynamical model demonstrating how interactions between sea ice and deep water formation can produce millennial-scale oscillations, explaining historical climate events like Dansgaard-Oeschger and Bond events.

Contribution

It proposes a novel auto-oscillatory mechanism linking sea ice and convection, supported by a coupled dynamical model that reproduces observed climate oscillations and their modulation by freshwater and insolation.

Findings

Model exhibits mixed mode oscillations with decadal and millennial scales.

Freshwater pulses cause oscillation grouping similar to proxy records.

Mechanism potentially explains timing and pacing of past climate events.

Abstract

During the last ice age there were several quasi-periodic abrupt warming events. The climatic effects of the so-called Dansgaard-Oeschger (DO) events were felt globally, although the North Atlantic experienced the largest and most abrupt temperature anomalies. Similar but weaker oscillations also took place during the interglacial period. This paper proposes an auto-oscillatory mechanism between sea ice and convective deep water formation in the north Atlantic as the source of the persistent cycles. A simple dynamical model is constructed by coupling and slightly modifying two existing models of ocean circulation and sea ice. The model exhibits mixed mode oscillations, consisting of decadal scale small amplitude oscillations, and a large amplitude relaxation fluctuation. The decadal oscillations occur due to the insulating effect of sea ice and leads to periodic ventilation of heat from the polar ocean. Gradually an instability builds up in the polar column and results in an abrupt initiation of convection and polar warming. The unstable convective state relaxes back to the small amplitude oscillations from where the process repeats in a self-sustained manner. Freshwater pulses mimicking Heinrich events cause the oscillations to be grouped into packets of progressively weaker fluctuations, as also observed in the proxy records. Modulation of this stable oscillation mechanism by freshwater and insolation variations could account for the distribution and pacing of DO and Bond events. Physical aspects of the system such as sea ice extent and oceanic advective flow rates could determine the characteristic 1,500 year timescale of DO events.