Abstract
The time-dependent properties of the Fokker–Planck equation corresponding to a zero-dimensional climate model, showing bistable behavior and subject to a weak external periodic forcing are analyzed. Conditions under which the response is amplified are found analytically. In this way the possibility of transitions between climatic states is established. The results are illustrated by the 100,000-yr periodicity of the eccentricity of the earth's orbit, in connection with glaciation cycles.
DOI: https://doi.org/10.3402/tellusa.v34i1.10781 | Journal eISSN: 3035-9554
Language: English
Page range: 1 - 9
Submitted on: Feb 20, 1981
Published on: Jan 1, 1982
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1982 C. Nicolis, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
