UVic earth system climate model data generated under MIS3 boundary conditions ...
The modelling dataset presented here corresponds to the study entitled "Transient response of Southern Ocean ecosystems during Heinrich stadials". Antarctic ice core records suggest that atmospheric CO2 increased by 15 to 20 ppm during Heinrich stadials (HS). These periods of abrupt CO2 in...
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Online Access: | https://dx.doi.org/10.5061/dryad.k3j9kd5dt https://datadryad.org/stash/dataset/doi:10.5061/dryad.k3j9kd5dt |
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ftdatacite:10.5061/dryad.k3j9kd5dt 2024-03-31T07:48:14+00:00 UVic earth system climate model data generated under MIS3 boundary conditions ... Saini, Himadri Meissner, Katrin J. Kvale, Karin Menviel, Laurie 2023 https://dx.doi.org/10.5061/dryad.k3j9kd5dt https://datadryad.org/stash/dataset/doi:10.5061/dryad.k3j9kd5dt en eng Dryad Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 FOS Earth and related environmental sciences Heinrich stadiums Atlantic Meridional Overturning Circulation Marine ecosystems iron fertilisation dataset Dataset 2023 ftdatacite https://doi.org/10.5061/dryad.k3j9kd5dt 2024-03-04T11:45:31Z The modelling dataset presented here corresponds to the study entitled "Transient response of Southern Ocean ecosystems during Heinrich stadials". Antarctic ice core records suggest that atmospheric CO2 increased by 15 to 20 ppm during Heinrich stadials (HS). These periods of abrupt CO2 increase are associated with a significant weakening of the Atlantic meridional overturning circulation (AMOC), and a warming at high southern latitudes. As such, modelling studies have explored the link between changes in AMOC, high southern latitude climate and atmospheric CO2. While proxy records suggest that the aeolian iron input to the Southern Ocean decreased significantly during HS, the potential impact on CO2 of reduced iron input combined with oceanic circulation changes has not been studied in detail. Here, we quantify the respective and combined impacts of reduced iron fertilisation and AMOC weakening on CO2 by performing numerical experiments with an Earth system model under boundary conditions representing ... : The data is generated through modelling simulations using the University of Victoria Earth system climate model. ... Dataset Antarc* Antarctic ice core Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Southern Ocean |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
English |
topic |
FOS Earth and related environmental sciences Heinrich stadiums Atlantic Meridional Overturning Circulation Marine ecosystems iron fertilisation |
spellingShingle |
FOS Earth and related environmental sciences Heinrich stadiums Atlantic Meridional Overturning Circulation Marine ecosystems iron fertilisation Saini, Himadri Meissner, Katrin J. Kvale, Karin Menviel, Laurie UVic earth system climate model data generated under MIS3 boundary conditions ... |
topic_facet |
FOS Earth and related environmental sciences Heinrich stadiums Atlantic Meridional Overturning Circulation Marine ecosystems iron fertilisation |
description |
The modelling dataset presented here corresponds to the study entitled "Transient response of Southern Ocean ecosystems during Heinrich stadials". Antarctic ice core records suggest that atmospheric CO2 increased by 15 to 20 ppm during Heinrich stadials (HS). These periods of abrupt CO2 increase are associated with a significant weakening of the Atlantic meridional overturning circulation (AMOC), and a warming at high southern latitudes. As such, modelling studies have explored the link between changes in AMOC, high southern latitude climate and atmospheric CO2. While proxy records suggest that the aeolian iron input to the Southern Ocean decreased significantly during HS, the potential impact on CO2 of reduced iron input combined with oceanic circulation changes has not been studied in detail. Here, we quantify the respective and combined impacts of reduced iron fertilisation and AMOC weakening on CO2 by performing numerical experiments with an Earth system model under boundary conditions representing ... : The data is generated through modelling simulations using the University of Victoria Earth system climate model. ... |
format |
Dataset |
author |
Saini, Himadri Meissner, Katrin J. Kvale, Karin Menviel, Laurie |
author_facet |
Saini, Himadri Meissner, Katrin J. Kvale, Karin Menviel, Laurie |
author_sort |
Saini, Himadri |
title |
UVic earth system climate model data generated under MIS3 boundary conditions ... |
title_short |
UVic earth system climate model data generated under MIS3 boundary conditions ... |
title_full |
UVic earth system climate model data generated under MIS3 boundary conditions ... |
title_fullStr |
UVic earth system climate model data generated under MIS3 boundary conditions ... |
title_full_unstemmed |
UVic earth system climate model data generated under MIS3 boundary conditions ... |
title_sort |
uvic earth system climate model data generated under mis3 boundary conditions ... |
publisher |
Dryad |
publishDate |
2023 |
url |
https://dx.doi.org/10.5061/dryad.k3j9kd5dt https://datadryad.org/stash/dataset/doi:10.5061/dryad.k3j9kd5dt |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic ice core Southern Ocean |
genre_facet |
Antarc* Antarctic ice core Southern Ocean |
op_rights |
Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode cc0-1.0 |
op_doi |
https://doi.org/10.5061/dryad.k3j9kd5dt |
_version_ |
1795029771484135424 |