A Discontinuous ODE Model of the Glacial Cycles with Diffusive Heat Transport
We present a new discontinuous ordinary differential equation (ODE) model of the glacial cycles. Model trajectories flip from a glacial to an interglacial state, and vice versa, via a switching mechanism motivated by ice sheet mass balance principles. Filippov’s theory of differential incl...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-03-01
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Series: | Mathematics |
Subjects: | |
Online Access: | https://www.mdpi.com/2227-7390/8/3/316 |