ESD Ideas: Propagation of high-frequency forcing to ice age dynamics
Palaeoclimate records display a continuous background of variability connecting centennial to 100 kyr periods. Hence, the dynamics at the centennial, millennial, and astronomical timescales should not be treated separately. Here, we show that the nonlinear character of ice sheet dynamics, which was...
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ftdoajarticles:oai:doaj.org/article:4e2ffa69ad724a098f73de87ec53778c 2023-05-15T16:40:30+02:00 ESD Ideas: Propagation of high-frequency forcing to ice age dynamics M. Y. Verbitsky M. Crucifix D. M. Volobuev 2019-04-01T00:00:00Z https://doi.org/10.5194/esd-10-257-2019 https://doaj.org/article/4e2ffa69ad724a098f73de87ec53778c EN eng Copernicus Publications https://www.earth-syst-dynam.net/10/257/2019/esd-10-257-2019.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-10-257-2019 2190-4979 2190-4987 https://doaj.org/article/4e2ffa69ad724a098f73de87ec53778c Earth System Dynamics, Vol 10, Pp 257-260 (2019) Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 article 2019 ftdoajarticles https://doi.org/10.5194/esd-10-257-2019 2022-12-30T21:34:00Z Palaeoclimate records display a continuous background of variability connecting centennial to 100 kyr periods. Hence, the dynamics at the centennial, millennial, and astronomical timescales should not be treated separately. Here, we show that the nonlinear character of ice sheet dynamics, which was derived naturally from the ice-flow conservation laws, provides the scaling constraints to explain the structure of the observed spectrum of variability. Article in Journal/Newspaper Ice Sheet Directory of Open Access Journals: DOAJ Articles Earth System Dynamics 10 2 257 260 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
spellingShingle |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 M. Y. Verbitsky M. Crucifix D. M. Volobuev ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
topic_facet |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
description |
Palaeoclimate records display a continuous background of variability connecting centennial to 100 kyr periods. Hence, the dynamics at the centennial, millennial, and astronomical timescales should not be treated separately. Here, we show that the nonlinear character of ice sheet dynamics, which was derived naturally from the ice-flow conservation laws, provides the scaling constraints to explain the structure of the observed spectrum of variability. |
format |
Article in Journal/Newspaper |
author |
M. Y. Verbitsky M. Crucifix D. M. Volobuev |
author_facet |
M. Y. Verbitsky M. Crucifix D. M. Volobuev |
author_sort |
M. Y. Verbitsky |
title |
ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
title_short |
ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
title_full |
ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
title_fullStr |
ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
title_full_unstemmed |
ESD Ideas: Propagation of high-frequency forcing to ice age dynamics |
title_sort |
esd ideas: propagation of high-frequency forcing to ice age dynamics |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/esd-10-257-2019 https://doaj.org/article/4e2ffa69ad724a098f73de87ec53778c |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Earth System Dynamics, Vol 10, Pp 257-260 (2019) |
op_relation |
https://www.earth-syst-dynam.net/10/257/2019/esd-10-257-2019.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-10-257-2019 2190-4979 2190-4987 https://doaj.org/article/4e2ffa69ad724a098f73de87ec53778c |
op_doi |
https://doi.org/10.5194/esd-10-257-2019 |
container_title |
Earth System Dynamics |
container_volume |
10 |
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2 |
container_start_page |
257 |
op_container_end_page |
260 |
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1766030899968737280 |