Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures

This paper describes differences between Medieval Climate Anomaly (MCA) and present-day temperatures in the area composed of the Antarctic Peninsula, southern Patagonia, and the surrounding southern oceans. The investigation is conducted with the simulation results from the Community Earth System Mo...

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Published in:Quaternary Science Reviews
Main Authors: Silvestri, Gabriel Emilio, Berman, Ana Laura, de Vleeschouwer, Francois, Wainer, Ilana
Format: Article in Journal/Newspaper
Language:English
Published: Pergamon-Elsevier Science Ltd
Subjects:
Online Access:http://hdl.handle.net/11336/180993
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record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/180993 2023-10-09T21:47:09+02:00 Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures Silvestri, Gabriel Emilio Berman, Ana Laura de Vleeschouwer, Francois Wainer, Ilana application/pdf http://hdl.handle.net/11336/180993 eng eng Pergamon-Elsevier Science Ltd info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0277379121004807 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2021.107273 http://hdl.handle.net/11336/180993 Silvestri, Gabriel Emilio; Berman, Ana Laura; de Vleeschouwer, Francois; Wainer, Ilana; Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 274; 11-2021; 1-12 0277-3791 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ANTARCTIC PENINSULA CESM-LME SIMULATIONS LAST MILLENNIUM LITTLE ICE AGE MEDIEVAL CLIMATE ANOMALY PATAGONIA https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.quascirev.2021.107273 2023-09-24T18:36:59Z This paper describes differences between Medieval Climate Anomaly (MCA) and present-day temperatures in the area composed of the Antarctic Peninsula, southern Patagonia, and the surrounding southern oceans. The investigation is conducted with the simulation results from the Community Earth System Model Last Millennium Ensemble (CESM-LME) considering the impact of each natural (volcanic activity and solar variability) and anthropogenic (greenhouse gas, ozone-aerosols and land use/land cover) individual forcing relative to the full forced simulations. Model results show generalized warming during the MCA in the study area. However, the simulated MCA temperatures are significantly colder than present-day mean values due to the influence of increased atmospheric greenhouse gas concentrations since the beginning of the modern Industrial Era in the ∼1850s. In fact, model runs in which only natural forcings were applied show that, in the absence of greenhouse gas forcing, present-day temperatures in the Antarctic Peninsula and southern Patagonia would be lower than or similar to those during the MCA. The study demonstrates the value of paleoclimate proxy–model comparisons but also highlights the limitations of current available proxy information to perform that integration in the study area. Fil: Silvestri, Gabriel Emilio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina Fil: Berman, Ana Laura. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina Fil: de Vleeschouwer, Francois. Centre National de la Recherche ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Antarctic Peninsula Patagonia Argentina Quaternary Science Reviews 274 107273
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic ANTARCTIC PENINSULA
CESM-LME SIMULATIONS
LAST MILLENNIUM
LITTLE ICE AGE
MEDIEVAL CLIMATE ANOMALY
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle ANTARCTIC PENINSULA
CESM-LME SIMULATIONS
LAST MILLENNIUM
LITTLE ICE AGE
MEDIEVAL CLIMATE ANOMALY
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Silvestri, Gabriel Emilio
Berman, Ana Laura
de Vleeschouwer, Francois
Wainer, Ilana
Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
topic_facet ANTARCTIC PENINSULA
CESM-LME SIMULATIONS
LAST MILLENNIUM
LITTLE ICE AGE
MEDIEVAL CLIMATE ANOMALY
PATAGONIA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description This paper describes differences between Medieval Climate Anomaly (MCA) and present-day temperatures in the area composed of the Antarctic Peninsula, southern Patagonia, and the surrounding southern oceans. The investigation is conducted with the simulation results from the Community Earth System Model Last Millennium Ensemble (CESM-LME) considering the impact of each natural (volcanic activity and solar variability) and anthropogenic (greenhouse gas, ozone-aerosols and land use/land cover) individual forcing relative to the full forced simulations. Model results show generalized warming during the MCA in the study area. However, the simulated MCA temperatures are significantly colder than present-day mean values due to the influence of increased atmospheric greenhouse gas concentrations since the beginning of the modern Industrial Era in the ∼1850s. In fact, model runs in which only natural forcings were applied show that, in the absence of greenhouse gas forcing, present-day temperatures in the Antarctic Peninsula and southern Patagonia would be lower than or similar to those during the MCA. The study demonstrates the value of paleoclimate proxy–model comparisons but also highlights the limitations of current available proxy information to perform that integration in the study area. Fil: Silvestri, Gabriel Emilio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina Fil: Berman, Ana Laura. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de Investigaciones del Mar y la Atmósfera; Argentina Fil: de Vleeschouwer, Francois. Centre National de la Recherche ...
format Article in Journal/Newspaper
author Silvestri, Gabriel Emilio
Berman, Ana Laura
de Vleeschouwer, Francois
Wainer, Ilana
author_facet Silvestri, Gabriel Emilio
Berman, Ana Laura
de Vleeschouwer, Francois
Wainer, Ilana
author_sort Silvestri, Gabriel Emilio
title Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
title_short Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
title_full Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
title_fullStr Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
title_full_unstemmed Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures
title_sort last millennium climate changes over the antarctic peninsula and southern patagonia in cesm-lme simulations: differences between medieval climate anomaly and present-day temperatures
publisher Pergamon-Elsevier Science Ltd
url http://hdl.handle.net/11336/180993
geographic Antarctic
The Antarctic
Antarctic Peninsula
Patagonia
Argentina
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Patagonia
Argentina
genre Antarc*
Antarctic
Antarctic Peninsula
genre_facet Antarc*
Antarctic
Antarctic Peninsula
op_relation info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0277379121004807
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2021.107273
http://hdl.handle.net/11336/180993
Silvestri, Gabriel Emilio; Berman, Ana Laura; de Vleeschouwer, Francois; Wainer, Ilana; Last millennium climate changes over the Antarctic Peninsula and southern Patagonia in CESM-LME simulations: differences between Medieval Climate Anomaly and present-day temperatures; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 274; 11-2021; 1-12
0277-3791
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/restrictedAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
op_doi https://doi.org/10.1016/j.quascirev.2021.107273
container_title Quaternary Science Reviews
container_volume 274
container_start_page 107273
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