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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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) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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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 |
_version_ |
1766031234931097600 |