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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Bibliographic Details
Main Authors: Saini, Himadri, Meissner, Katrin J., Kvale, Karin, Menviel, Laurie
Format: Dataset
Language:English
Published: Dryad 2023
Subjects:
Online Access:https://dx.doi.org/10.5061/dryad.k3j9kd5dt
https://datadryad.org/stash/dataset/doi:10.5061/dryad.k3j9kd5dt
id ftdatacite:10.5061/dryad.k3j9kd5dt
record_format openpolar
spelling 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
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id 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