A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records

Spectral analyses performed on records of cosmogenic nuclides reveal a group of dominant spectral components during the Holocene period. Only a few of them are related to known solar cycles, i.e., the De Vries/Suess, Gleissberg and Hallstatt cycles. The origin of the others remains uncertain. On the...

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Main Authors: Quiroga Lombard, C.S., Balenzuela, P., Braun, H., Chialvo, D.R.
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
Online Access:https://hdl.handle.net/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard
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spelling ftunibueairesbd:paperaa:paper_10235809_v17_n5_p585_QuirogaLombard 2023-05-15T15:09:23+02:00 A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records Quiroga Lombard, C.S. Balenzuela, P. Braun, H. Chialvo, D.R. 2010 application/pdf https://hdl.handle.net/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard eng eng http://hdl.handle.net/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar CC-BY Nonlinear Processes Geophys. 2010;17(5):585-592 air temperature Holocene paleoclimate paleotemperature proxy climate record sea surface temperature spectral analysis Arctic Atlantic Ocean Atlantic Ocean (North) Greenland Greenland Ice Sheet info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion 2010 ftunibueairesbd https://doi.org/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard 2023-02-16T01:51:57Z Spectral analyses performed on records of cosmogenic nuclides reveal a group of dominant spectral components during the Holocene period. Only a few of them are related to known solar cycles, i.e., the De Vries/Suess, Gleissberg and Hallstatt cycles. The origin of the others remains uncertain. On the other hand, time series of North Atlantic atmospheric/sea surface temperatures during the last ice age display the existence of repeated large-scale warming events, called Dansgaard-Oeschger (DO) events, spaced around multiples of 1470 years. The De Vries/Suess and Gleissberg cycles with periods close to 1470/7 (∼210) and 1470/17 (∼86.5) years have been proposed to explain these observations. In this work we found that a conceptual bistable model forced with the De Vries/Suess and Gleissberg cycles plus noise displays a group of dominant frequencies similar to those obtained in the Fourier spectra from paleo-climate during the Holocene. Moreover, we show that simply changing the noise amplitude in the model we obtain similar power spectra to those corresponding to GISP2 δ18O (Greenland Ice Sheet Project 2) during the last ice age. These results give a general dynamical framework which allows us to interpret the main characteristic of paleoclimate records from the last 100 000 years. © 2010 Author(s). Fil:Balenzuela, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Article in Journal/Newspaper Arctic Greenland Greenland Ice Sheet Project Ice Sheet North Atlantic North Greenland Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Arctic Argentina Greenland
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language English
topic air temperature
Holocene
paleoclimate
paleotemperature
proxy climate record
sea surface temperature
spectral analysis
Arctic
Atlantic Ocean
Atlantic Ocean (North)
Greenland
Greenland Ice Sheet
spellingShingle air temperature
Holocene
paleoclimate
paleotemperature
proxy climate record
sea surface temperature
spectral analysis
Arctic
Atlantic Ocean
Atlantic Ocean (North)
Greenland
Greenland Ice Sheet
Quiroga Lombard, C.S.
Balenzuela, P.
Braun, H.
Chialvo, D.R.
A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
topic_facet air temperature
Holocene
paleoclimate
paleotemperature
proxy climate record
sea surface temperature
spectral analysis
Arctic
Atlantic Ocean
Atlantic Ocean (North)
Greenland
Greenland Ice Sheet
description Spectral analyses performed on records of cosmogenic nuclides reveal a group of dominant spectral components during the Holocene period. Only a few of them are related to known solar cycles, i.e., the De Vries/Suess, Gleissberg and Hallstatt cycles. The origin of the others remains uncertain. On the other hand, time series of North Atlantic atmospheric/sea surface temperatures during the last ice age display the existence of repeated large-scale warming events, called Dansgaard-Oeschger (DO) events, spaced around multiples of 1470 years. The De Vries/Suess and Gleissberg cycles with periods close to 1470/7 (∼210) and 1470/17 (∼86.5) years have been proposed to explain these observations. In this work we found that a conceptual bistable model forced with the De Vries/Suess and Gleissberg cycles plus noise displays a group of dominant frequencies similar to those obtained in the Fourier spectra from paleo-climate during the Holocene. Moreover, we show that simply changing the noise amplitude in the model we obtain similar power spectra to those corresponding to GISP2 δ18O (Greenland Ice Sheet Project 2) during the last ice age. These results give a general dynamical framework which allows us to interpret the main characteristic of paleoclimate records from the last 100 000 years. © 2010 Author(s). Fil:Balenzuela, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
format Article in Journal/Newspaper
author Quiroga Lombard, C.S.
Balenzuela, P.
Braun, H.
Chialvo, D.R.
author_facet Quiroga Lombard, C.S.
Balenzuela, P.
Braun, H.
Chialvo, D.R.
author_sort Quiroga Lombard, C.S.
title A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
title_short A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
title_full A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
title_fullStr A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
title_full_unstemmed A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
title_sort simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records
publishDate 2010
url https://hdl.handle.net/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard
geographic Arctic
Argentina
Greenland
geographic_facet Arctic
Argentina
Greenland
genre Arctic
Greenland
Greenland Ice Sheet Project
Ice Sheet
North Atlantic
North Greenland
genre_facet Arctic
Greenland
Greenland Ice Sheet Project
Ice Sheet
North Atlantic
North Greenland
op_source Nonlinear Processes Geophys. 2010;17(5):585-592
op_relation http://hdl.handle.net/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
op_rightsnorm CC-BY
op_doi https://doi.org/20.500.12110/paper_10235809_v17_n5_p585_QuirogaLombard
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