Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia
The Leeuwin Current (LC), an eastern boundary current, transports tropical waters from the Indo-Pacific Warm Pool (IPWP) towards southern latitudes and modulates oceanic conditions offshore southern Australia. New, high-resolution planktic foraminifer assemblage data and alkenone-derived sea surface...
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/232672 2024-01-14T10:09:13+01:00 Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia Perner, Kerstin Moros, Matthias De Deckker, Patrick Blanz, Thomas Wacker, Lukas Telford, Richard J. Siegel, Herbert Schneider, Ralph Jansen, Eystein application/pdf http://hdl.handle.net/1885/232672 https://doi.org/10.1016/j.quascirev.2017.11.033 https://openresearch-repository.anu.edu.au/bitstream/1885/232672/3/01_Perner_Heat_export_from_the_tropics_2018.pdf.jpg en_AU eng Pergamon-Elsevier Ltd http://purl.org/au-research/grants/arc/DP0344932 0277-3791 http://hdl.handle.net/1885/232672 doi:10.1016/j.quascirev.2017.11.033 https://openresearch-repository.anu.edu.au/bitstream/1885/232672/3/01_Perner_Heat_export_from_the_tropics_2018.pdf.jpg © 2017 Elsevier Ltd. Quaternary Science Reviews Planktic foraminifer Sea surface temperature Palaeoceanography ENSO Holocene Southern Ocean Australia Journal article ftanucanberra https://doi.org/10.1016/j.quascirev.2017.11.033 2023-12-15T09:34:03Z The Leeuwin Current (LC), an eastern boundary current, transports tropical waters from the Indo-Pacific Warm Pool (IPWP) towards southern latitudes and modulates oceanic conditions offshore southern Australia. New, high-resolution planktic foraminifer assemblage data and alkenone-derived sea surface temperatures (SST) provide an in-depth view on LC variability and mechanisms driving the current's properties during the mid to late Holocene (last c. 7.4 ka BP). Our marine reconstructions highlight a longer-term mid to late Holocene reduction of tropical heat export from the IPWP area into the LC. Mid Holocene (c. 7.4 to 3.5 ka BP) occurrence of high SSTs (>19.5 °C), tropical planktic foraminifera and a well-stratified water column document an enhanced heat export from the tropics. From c. 3.5 ka BP onwards, a weaker LC and a notably reduced tropical heat export cause oceanic cooling offshore southern Australia. The observed mid to late Holocene trends likely result from large-scale changes in the IPWP's heat storage linked to the El Niño-Southern Oscillation (ENSO) phenomenon. We propose that a strong and warm LC occurs in response to a La Niña-like state of ENSO during the mid Holocene. The late Holocene LC cooling, however, results from a shift towards an El Niño-like state and a more variable ENSO system that causes cooling of the IPWP. Superimposed on these longer-term trends we find evidence of distinct late Holocene millennial-scale phases of enhanced El Niño/La Niña development, which appear synchronous with northern hemispheric climatic variability. Phases of dominant El Niño-like states occur parallel to North Atlantic cold phases: the ‘2800 years BP cooling event’, the ‘Dark Ages’ and the ‘Little Ice Age’, whereas the ‘Roman Warm Period’ and the ‘Medieval Climate Anomaly’ parallel periods of a predominant La Niña-like state. Our findings provide further evidence of coherent interhemispheric climatic and oceanic conditions during the mid to late Holocene, suggesting ENSO as a potential mediator. This ... Article in Journal/Newspaper North Atlantic Southern Ocean Australian National University: ANU Digital Collections Southern Ocean Pacific Quaternary Science Reviews 180 96 110 |
institution |
Open Polar |
collection |
Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
English |
topic |
Planktic foraminifer Sea surface temperature Palaeoceanography ENSO Holocene Southern Ocean Australia |
spellingShingle |
Planktic foraminifer Sea surface temperature Palaeoceanography ENSO Holocene Southern Ocean Australia Perner, Kerstin Moros, Matthias De Deckker, Patrick Blanz, Thomas Wacker, Lukas Telford, Richard J. Siegel, Herbert Schneider, Ralph Jansen, Eystein Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
topic_facet |
Planktic foraminifer Sea surface temperature Palaeoceanography ENSO Holocene Southern Ocean Australia |
description |
The Leeuwin Current (LC), an eastern boundary current, transports tropical waters from the Indo-Pacific Warm Pool (IPWP) towards southern latitudes and modulates oceanic conditions offshore southern Australia. New, high-resolution planktic foraminifer assemblage data and alkenone-derived sea surface temperatures (SST) provide an in-depth view on LC variability and mechanisms driving the current's properties during the mid to late Holocene (last c. 7.4 ka BP). Our marine reconstructions highlight a longer-term mid to late Holocene reduction of tropical heat export from the IPWP area into the LC. Mid Holocene (c. 7.4 to 3.5 ka BP) occurrence of high SSTs (>19.5 °C), tropical planktic foraminifera and a well-stratified water column document an enhanced heat export from the tropics. From c. 3.5 ka BP onwards, a weaker LC and a notably reduced tropical heat export cause oceanic cooling offshore southern Australia. The observed mid to late Holocene trends likely result from large-scale changes in the IPWP's heat storage linked to the El Niño-Southern Oscillation (ENSO) phenomenon. We propose that a strong and warm LC occurs in response to a La Niña-like state of ENSO during the mid Holocene. The late Holocene LC cooling, however, results from a shift towards an El Niño-like state and a more variable ENSO system that causes cooling of the IPWP. Superimposed on these longer-term trends we find evidence of distinct late Holocene millennial-scale phases of enhanced El Niño/La Niña development, which appear synchronous with northern hemispheric climatic variability. Phases of dominant El Niño-like states occur parallel to North Atlantic cold phases: the ‘2800 years BP cooling event’, the ‘Dark Ages’ and the ‘Little Ice Age’, whereas the ‘Roman Warm Period’ and the ‘Medieval Climate Anomaly’ parallel periods of a predominant La Niña-like state. Our findings provide further evidence of coherent interhemispheric climatic and oceanic conditions during the mid to late Holocene, suggesting ENSO as a potential mediator. This ... |
format |
Article in Journal/Newspaper |
author |
Perner, Kerstin Moros, Matthias De Deckker, Patrick Blanz, Thomas Wacker, Lukas Telford, Richard J. Siegel, Herbert Schneider, Ralph Jansen, Eystein |
author_facet |
Perner, Kerstin Moros, Matthias De Deckker, Patrick Blanz, Thomas Wacker, Lukas Telford, Richard J. Siegel, Herbert Schneider, Ralph Jansen, Eystein |
author_sort |
Perner, Kerstin |
title |
Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
title_short |
Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
title_full |
Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
title_fullStr |
Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
title_full_unstemmed |
Heat export from the tropics drives mid to late Holocene palaeoceanographic changes offshore southern Australia |
title_sort |
heat export from the tropics drives mid to late holocene palaeoceanographic changes offshore southern australia |
publisher |
Pergamon-Elsevier Ltd |
url |
http://hdl.handle.net/1885/232672 https://doi.org/10.1016/j.quascirev.2017.11.033 https://openresearch-repository.anu.edu.au/bitstream/1885/232672/3/01_Perner_Heat_export_from_the_tropics_2018.pdf.jpg |
geographic |
Southern Ocean Pacific |
geographic_facet |
Southern Ocean Pacific |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_source |
Quaternary Science Reviews |
op_relation |
http://purl.org/au-research/grants/arc/DP0344932 0277-3791 http://hdl.handle.net/1885/232672 doi:10.1016/j.quascirev.2017.11.033 https://openresearch-repository.anu.edu.au/bitstream/1885/232672/3/01_Perner_Heat_export_from_the_tropics_2018.pdf.jpg |
op_rights |
© 2017 Elsevier Ltd. |
op_doi |
https://doi.org/10.1016/j.quascirev.2017.11.033 |
container_title |
Quaternary Science Reviews |
container_volume |
180 |
container_start_page |
96 |
op_container_end_page |
110 |
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1788063694099316736 |