Abstract
The effect of a periodic forcing on the mean ocean temperature - sea ice system is analyzed in a region of parameters in which this latter system gives rise to a homoclinic bifurcation. The possibility of complex, nonperiodic behavior as well as of long period solutions is established both analytically and by numerical simulations. The implications of the results in the glaciation problem are briefly discussed.
DOI: https://doi.org/10.3402/tellusa.v39i1.11734 | Journal eISSN: 3035-9554
Language: English
Page range: 1 - 9
Submitted on: Nov 29, 1985
Accepted on: Feb 28, 1986
Published on: Jan 1, 1987
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1987 C. Nicolis, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
