A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data
A stochastic Duffing-type oscillator model, i.e noise-driven motion with inertia in a potential landscape, is considered for glacial millennial-scale climate transitions. The potential and noise parameters are estimated from a Greenland ice-core record using a nonlinear Kalman filter. For the period...
Published in: | Nonlinear Processes in Geophysics |
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Online Access: | https://doi.org/10.5194/npg-19-595-2012 https://npg.copernicus.org/articles/19/595/2012/ |
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ftcopernicus:oai:publications.copernicus.org:npg15619 2023-05-15T16:28:18+02:00 A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data Kwasniok, F. Lohmann, G. 2018-01-15 application/pdf https://doi.org/10.5194/npg-19-595-2012 https://npg.copernicus.org/articles/19/595/2012/ eng eng doi:10.5194/npg-19-595-2012 https://npg.copernicus.org/articles/19/595/2012/ eISSN: 1607-7946 Text 2018 ftcopernicus https://doi.org/10.5194/npg-19-595-2012 2020-07-20T16:25:39Z A stochastic Duffing-type oscillator model, i.e noise-driven motion with inertia in a potential landscape, is considered for glacial millennial-scale climate transitions. The potential and noise parameters are estimated from a Greenland ice-core record using a nonlinear Kalman filter. For the period from 60 to 20 ky before present, a bistable potential with a deep well corresponding to a cold stadial state and a shallow well corresponding to a warm interstadial state is found. The system is in the strongly dissipative regime and can be very well approximated by an effective one-dimensional Langevin equation. Text Greenland Greenland ice core ice core Copernicus Publications: E-Journals Greenland Nonlinear Processes in Geophysics 19 6 595 603 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
A stochastic Duffing-type oscillator model, i.e noise-driven motion with inertia in a potential landscape, is considered for glacial millennial-scale climate transitions. The potential and noise parameters are estimated from a Greenland ice-core record using a nonlinear Kalman filter. For the period from 60 to 20 ky before present, a bistable potential with a deep well corresponding to a cold stadial state and a shallow well corresponding to a warm interstadial state is found. The system is in the strongly dissipative regime and can be very well approximated by an effective one-dimensional Langevin equation. |
format |
Text |
author |
Kwasniok, F. Lohmann, G. |
spellingShingle |
Kwasniok, F. Lohmann, G. A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
author_facet |
Kwasniok, F. Lohmann, G. |
author_sort |
Kwasniok, F. |
title |
A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
title_short |
A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
title_full |
A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
title_fullStr |
A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
title_full_unstemmed |
A stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
title_sort |
stochastic nonlinear oscillator model for glacial millennial-scale climate transitions derived from ice-core data |
publishDate |
2018 |
url |
https://doi.org/10.5194/npg-19-595-2012 https://npg.copernicus.org/articles/19/595/2012/ |
geographic |
Greenland |
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Greenland |
genre |
Greenland Greenland ice core ice core |
genre_facet |
Greenland Greenland ice core ice core |
op_source |
eISSN: 1607-7946 |
op_relation |
doi:10.5194/npg-19-595-2012 https://npg.copernicus.org/articles/19/595/2012/ |
op_doi |
https://doi.org/10.5194/npg-19-595-2012 |
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Nonlinear Processes in Geophysics |
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19 |
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6 |
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595 |
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603 |
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1766017934993391616 |