Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles

The Late Pleistocene Antarctic temperature variation curve is decomposed into two parts: cyclic and stochastic. These two parts represent different but tightly interconnected processes and also represent two different types of self-organization of the Earth climate system. The self-organization in t...

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Bibliographic Details
Main Author: Maslov, Lev A.
Format: Report
Language:unknown
Published: arXiv 2014
Subjects:
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Antarctic
Antarc*
Online Access:https://dx.doi.org/10.48550/arxiv.1401.4652
https://arxiv.org/abs/1401.4652
id ftdatacite:10.48550/arxiv.1401.4652
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1401.4652 2023-05-15T13:59:13+02:00 Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles Maslov, Lev A. 2014 https://dx.doi.org/10.48550/arxiv.1401.4652 https://arxiv.org/abs/1401.4652 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Preprint Article article CreativeWork 2014 ftdatacite https://doi.org/10.48550/arxiv.1401.4652 2022-04-01T13:12:47Z The Late Pleistocene Antarctic temperature variation curve is decomposed into two parts: cyclic and stochastic. These two parts represent different but tightly interconnected processes and also represent two different types of self-organization of the Earth climate system. The self-organization in the cyclic component is the non-linear auto-oscillation reaction of the Earth climate system, as a whole, to the input of solar radiation. The self-organization in the stochastic component is a nonlinear critical process, taking energy from, and fluctuating around the cyclic component of the temperature variations. The system of ODEs is written to model the cyclic part of the temperature variation, and the multifractal spectrum of the stochastic part of the temperature variation is calculated. The Earth climate can be characterized as an open, complex, self-organized dynamical system with nonlinear reaction to the input of solar radiation. : This paper has been withdrawn by the author because of his disappointment in this work Report Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Maslov, Lev A.
Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
description The Late Pleistocene Antarctic temperature variation curve is decomposed into two parts: cyclic and stochastic. These two parts represent different but tightly interconnected processes and also represent two different types of self-organization of the Earth climate system. The self-organization in the cyclic component is the non-linear auto-oscillation reaction of the Earth climate system, as a whole, to the input of solar radiation. The self-organization in the stochastic component is a nonlinear critical process, taking energy from, and fluctuating around the cyclic component of the temperature variations. The system of ODEs is written to model the cyclic part of the temperature variation, and the multifractal spectrum of the stochastic part of the temperature variation is calculated. The Earth climate can be characterized as an open, complex, self-organized dynamical system with nonlinear reaction to the input of solar radiation. : This paper has been withdrawn by the author because of his disappointment in this work
format Report
author Maslov, Lev A.
author_facet Maslov, Lev A.
author_sort Maslov, Lev A.
title Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
title_short Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
title_full Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
title_fullStr Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
title_full_unstemmed Self-organization in the Earth climate system versus Milankovitch-Berger astronomical cycles
title_sort self-organization in the earth climate system versus milankovitch-berger astronomical cycles
publisher arXiv
publishDate 2014
url https://dx.doi.org/10.48550/arxiv.1401.4652
https://arxiv.org/abs/1401.4652
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1401.4652
_version_ 1766267726984118272

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