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Titel The dynamics of a low-order model for the Atlantic Multidecadal Oscillation
VerfasserIn Alef Sterk, Renato Vitolo, Henk Broer, Carles Simo, Henk Dijkstra
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250034543
 
Zusammenfassung
Observations and model studies provide ample evidence for the presence of multidecadal variability in the North Atlantic sea-surface temperature known as the Atlantic Multidecadal Oscillation (AMO). This variability is characterised by a multidecadal time scale, the westward propagation of temperature anomalies, and a phase difference between the anomalous meridional and zonal overturning circulations. We derive a low-order model which captures the characteristics of the AMO. The starting point is a minimal model consisting of a thermal wind balance and an equation for the advection of temperature in a 3-dimensional box-shaped ocean basin. The low-order model is obtained by an orthogonal projection onto a finite-dimensional function space. Flows are forced by restoring the sea surface temperature to an idealised atmospheric temperature profile with an equator-to-pole gradient ΔT as a control parameter. A second control parameter, γ, interpolates between restoring (γ = 0) and prescribed heat flux (γ = 1) conditions. For the standard values ΔT = 20-ˆ˜C and γ = 0 the low-order model has a stable equilibrium which corresponds to a steady ocean flow. By increasing the parameter γ from 0 to 1 this equilibrium becomes unstable through a supercritical Hopf bifurcation and we find a periodic attractor with the physical signature of the AMO. In turn, this attractor can bifurcate through (cascades of) period doublings when ΔT is increased. Next, we impose a time-periodic forcing, modelling annual variations in the ocean-atmosphere heat flux. In this setting the AMO appears through a Hopf-NeÄ­mark-Sacker bifurcation as an invariant 2-torus attractor. Hence, we have to study bifurcations of invariant tori. For ΔT -‰¥ 22-ˆ˜C the 2-torus associated with the AMO bifurcates through a sequence of quasi-periodic period doublings, which can give birth to strange attractors of quasi-periodic Hénon-like type.