Glacial Cycles and Milankovitch Forcing

Using a recent conceptual model of the glacial-interglacial cycles we present more evidence of Milankovitch cycles being the trigger for retreat and forming of ice sheets in the cycles. This model is based on a finite approximation of an infinite dimensional model which has three components: Budyko&...

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Main Author: Raghuraman, Shiv Priyam
Format: Report
Language:unknown
Published: arXiv 2015
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1511.06008
https://arxiv.org/abs/1511.06008
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spelling ftdatacite:10.48550/arxiv.1511.06008 2023-05-15T16:40:49+02:00 Glacial Cycles and Milankovitch Forcing Raghuraman, Shiv Priyam 2015 https://dx.doi.org/10.48550/arxiv.1511.06008 https://arxiv.org/abs/1511.06008 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph Dynamical Systems math.DS FOS Physical sciences FOS Mathematics Preprint Article article CreativeWork 2015 ftdatacite https://doi.org/10.48550/arxiv.1511.06008 2022-04-01T11:51:53Z Using a recent conceptual model of the glacial-interglacial cycles we present more evidence of Milankovitch cycles being the trigger for retreat and forming of ice sheets in the cycles. This model is based on a finite approximation of an infinite dimensional model which has three components: Budyko's energy balance model describing the annual mean temperatures at latitudes, Widiasih's ODE which describes the behavior of the edge of the ice sheet, and Walsh et al. who introduced a snow line to account for glacial accumulation and ablation zones. Certain variables in the model are made to depend on the Milankovitch cycles, in particular, the obliquity of the Earth's axis and the eccentricity of the Earth's orbit. We see as a result that deglaciation and glaciation do occur mostly due to obliquity and to some extent eccentricity. Report Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
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
Dynamical Systems math.DS
FOS Physical sciences
FOS Mathematics
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
Dynamical Systems math.DS
FOS Physical sciences
FOS Mathematics
Raghuraman, Shiv Priyam
Glacial Cycles and Milankovitch Forcing
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
Dynamical Systems math.DS
FOS Physical sciences
FOS Mathematics
description Using a recent conceptual model of the glacial-interglacial cycles we present more evidence of Milankovitch cycles being the trigger for retreat and forming of ice sheets in the cycles. This model is based on a finite approximation of an infinite dimensional model which has three components: Budyko's energy balance model describing the annual mean temperatures at latitudes, Widiasih's ODE which describes the behavior of the edge of the ice sheet, and Walsh et al. who introduced a snow line to account for glacial accumulation and ablation zones. Certain variables in the model are made to depend on the Milankovitch cycles, in particular, the obliquity of the Earth's axis and the eccentricity of the Earth's orbit. We see as a result that deglaciation and glaciation do occur mostly due to obliquity and to some extent eccentricity.
format Report
author Raghuraman, Shiv Priyam
author_facet Raghuraman, Shiv Priyam
author_sort Raghuraman, Shiv Priyam
title Glacial Cycles and Milankovitch Forcing
title_short Glacial Cycles and Milankovitch Forcing
title_full Glacial Cycles and Milankovitch Forcing
title_fullStr Glacial Cycles and Milankovitch Forcing
title_full_unstemmed Glacial Cycles and Milankovitch Forcing
title_sort glacial cycles and milankovitch forcing
publisher arXiv
publishDate 2015
url https://dx.doi.org/10.48550/arxiv.1511.06008
https://arxiv.org/abs/1511.06008
genre Ice Sheet
genre_facet Ice Sheet
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1511.06008
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