Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation?
Instrumental records of the North Atlantic sea surface temperature reveal a large-scale low frequency mode of variability that has become known as the Atlantic Multidecadal Oscillation (AMO). Proxy and modelling studies have demonstrated the important consequences of the AMO on other components of t...
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ftdoajarticles:oai:doaj.org/article:7c09c69be02a4d108f4a846ac542f206 2023-05-15T17:34:06+02:00 Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? D. Heslop A. Paul 2011-03-01T00:00:00Z https://doi.org/10.5194/cp-7-151-2011 https://doaj.org/article/7c09c69be02a4d108f4a846ac542f206 EN eng Copernicus Publications http://www.clim-past.net/7/151/2011/cp-7-151-2011.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-7-151-2011 1814-9324 1814-9332 https://doaj.org/article/7c09c69be02a4d108f4a846ac542f206 Climate of the Past, Vol 7, Iss 1, Pp 151-159 (2011) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2011 ftdoajarticles https://doi.org/10.5194/cp-7-151-2011 2022-12-31T05:16:07Z Instrumental records of the North Atlantic sea surface temperature reveal a large-scale low frequency mode of variability that has become known as the Atlantic Multidecadal Oscillation (AMO). Proxy and modelling studies have demonstrated the important consequences of the AMO on other components of the climate system both within and outside the Atlantic region. Over longer time scales, the past behavior of the AMO is predominantly constrained by terrestrial proxies and only a limited number of records are available from the marine realm itself. Here we use an Earth System-Climate Model of intermediate complexity to simulate AMO-type behavior in the Atlantic with a specific focus placed on the ability of ocean paleothermometers to capture the associated surface and subsurface temperature variability. Given their lower prediction errors and annual resolution, coral-based proxies of sea surface temperature appear to be capable of reconstructing the temperature variations associated with the past AMO with an adequate signal-to-noise ratio. In contrast, the relatively high prediction error and low temporal resolution of sediment-based proxies, such as the composition of foraminiferal calcite, limits their ability to produce interpretable records of past temperature anomalies corresponding to AMO activity. Whilst the presented results will inevitably be model-dependent to some degree, the statistical framework is model-independent and can be applied to a wide variety of scenarios. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Climate of the Past 7 1 151 159 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
spellingShingle |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 D. Heslop A. Paul Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
topic_facet |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
description |
Instrumental records of the North Atlantic sea surface temperature reveal a large-scale low frequency mode of variability that has become known as the Atlantic Multidecadal Oscillation (AMO). Proxy and modelling studies have demonstrated the important consequences of the AMO on other components of the climate system both within and outside the Atlantic region. Over longer time scales, the past behavior of the AMO is predominantly constrained by terrestrial proxies and only a limited number of records are available from the marine realm itself. Here we use an Earth System-Climate Model of intermediate complexity to simulate AMO-type behavior in the Atlantic with a specific focus placed on the ability of ocean paleothermometers to capture the associated surface and subsurface temperature variability. Given their lower prediction errors and annual resolution, coral-based proxies of sea surface temperature appear to be capable of reconstructing the temperature variations associated with the past AMO with an adequate signal-to-noise ratio. In contrast, the relatively high prediction error and low temporal resolution of sediment-based proxies, such as the composition of foraminiferal calcite, limits their ability to produce interpretable records of past temperature anomalies corresponding to AMO activity. Whilst the presented results will inevitably be model-dependent to some degree, the statistical framework is model-independent and can be applied to a wide variety of scenarios. |
format |
Article in Journal/Newspaper |
author |
D. Heslop A. Paul |
author_facet |
D. Heslop A. Paul |
author_sort |
D. Heslop |
title |
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
title_short |
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
title_full |
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
title_fullStr |
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
title_full_unstemmed |
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation? |
title_sort |
can oceanic paleothermometers reconstruct the atlantic multidecadal oscillation? |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/cp-7-151-2011 https://doaj.org/article/7c09c69be02a4d108f4a846ac542f206 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Climate of the Past, Vol 7, Iss 1, Pp 151-159 (2011) |
op_relation |
http://www.clim-past.net/7/151/2011/cp-7-151-2011.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-7-151-2011 1814-9324 1814-9332 https://doaj.org/article/7c09c69be02a4d108f4a846ac542f206 |
op_doi |
https://doi.org/10.5194/cp-7-151-2011 |
container_title |
Climate of the Past |
container_volume |
7 |
container_issue |
1 |
container_start_page |
151 |
op_container_end_page |
159 |
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1766132827153235968 |