Synchronous Glacial Cycles in a Nonsmooth Conceptual Climate Model with Asymmetric Hemispheres
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Publication:5023530
DOI10.1137/21M1390098zbMath1489.37098arXiv2101.01707OpenAlexW3120818140MaRDI QIDQ5023530
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Publication date: 24 January 2022
Published in: SIAM Journal on Applied Dynamical Systems (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/2101.01707
ice-albedo feedbackpaleoclimatenonsmooth dynamical systemsglacial cyclesnonsmooth return mapvirtual equilibria
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Cites Work
- On the Budyko-Sellers energy balance climate model with ice line coupling
- Nonsmooth frameworks for an extended Budyko model
- Dynamics and bifurcations of non-smooth mechanical systems
- Piecewise linear differential systems without equilibria produce limit cycles?
- Dynamical systems analysis of the Maasch-Saltzman model for glacial cycles
- Limit cycles for regularized discontinuous dynamical systems with a hyperplane of discontinuity
- Piecewise-smooth dynamical systems. Theory and applications
- On continuous approximation of discontinuous systems
- Approximating annual mean incoming solar radiation
- Periodic orbits for a discontinuous vector field arising from a conceptual model of glacial cycles
- Dynamics of the Budyko Energy Balance Model
- A Quadratic Approximation to Budyko's Ice-Albedo Feedback Model with Ice Line Dynamics
- A Paleoclimate Model of Ice-Albedo Feedback Forced by Variations in Earth's Orbit
- An analysis of the periodically forced PP04 climate model, using the theory of non-smooth dynamical systems
- Bifurcation Sets of Continuous Piecewise Linear Systems with Two Zones
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