Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations

It is widely believed that multi-decadal to centennial cooling and drought occurred from 4500 to 3900 BP, known as the 4.2 ka BP event that triggered the collapse of several cultures. However, whether this event was a global event or a regional event and what caused this event remains unclear. In th...

Full description

Bibliographic Details
Published in:Climate of the Past
Main Authors: Yan, Mi, Liu, Jian
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Online Access:https://doi.org/10.5194/cp-15-265-2019
https://noa.gwlb.de/receive/cop_mods_00003207
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003165/cp-15-265-2019.pdf
https://cp.copernicus.org/articles/15/265/2019/cp-15-265-2019.pdf
id ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00003207
record_format openpolar
spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00003207 2023-05-15T17:35:23+02:00 Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations Yan, Mi Liu, Jian 2019-02 electronic https://doi.org/10.5194/cp-15-265-2019 https://noa.gwlb.de/receive/cop_mods_00003207 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003165/cp-15-265-2019.pdf https://cp.copernicus.org/articles/15/265/2019/cp-15-265-2019.pdf eng eng Copernicus Publications Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332 https://doi.org/10.5194/cp-15-265-2019 https://noa.gwlb.de/receive/cop_mods_00003207 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003165/cp-15-265-2019.pdf https://cp.copernicus.org/articles/15/265/2019/cp-15-265-2019.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2019 ftnonlinearchiv https://doi.org/10.5194/cp-15-265-2019 2022-02-08T23:00:42Z It is widely believed that multi-decadal to centennial cooling and drought occurred from 4500 to 3900 BP, known as the 4.2 ka BP event that triggered the collapse of several cultures. However, whether this event was a global event or a regional event and what caused this event remains unclear. In this study, we investigated the spatiotemporal characteristics, the possible causes and the related physical processes of the event using a set of long-term climate simulations, including one all-forcing experiment and four single-forcing experiments. The results derived from the all-forcing experiment show that this event occurs over most parts of the Northern Hemisphere (NH), indicating that this event could have been a hemispheric event. The cooler NH and warmer Southern Hemisphere (SH) illustrate that this event could be related to the slowdown of the Atlantic Meridional Overturning Circulation (AMOC). The comparison between the all-forcing experiment and the single-forcing experiments indicates that this event might have been caused by internal variability, while external forcings such as orbital and greenhouse gases might have modulation effects. A positive North Atlantic Oscillation (NAO)-like pattern in the atmosphere (low troposphere) triggered a negative Atlantic Multi-decadal Oscillation (AMO)-like pattern in the ocean, which then triggered a circum-global teleconnection (CGT)-like wave train pattern in the atmosphere (high troposphere). The positive NAO-like pattern and the CGT-like pattern are the direct physical processes that led to the NH cooling and mega-drought. The AMO-like pattern played a “bridge” role in maintaining this barotropic structure in the atmosphere at a multi-decadal–centennial timescale. Our work provides a global image and dynamic background to help better understand the 4.2 ka BP event. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Niedersächsisches Online-Archiv NOA Climate of the Past 15 1 265 277
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Yan, Mi
Liu, Jian
Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
topic_facet article
Verlagsveröffentlichung
description It is widely believed that multi-decadal to centennial cooling and drought occurred from 4500 to 3900 BP, known as the 4.2 ka BP event that triggered the collapse of several cultures. However, whether this event was a global event or a regional event and what caused this event remains unclear. In this study, we investigated the spatiotemporal characteristics, the possible causes and the related physical processes of the event using a set of long-term climate simulations, including one all-forcing experiment and four single-forcing experiments. The results derived from the all-forcing experiment show that this event occurs over most parts of the Northern Hemisphere (NH), indicating that this event could have been a hemispheric event. The cooler NH and warmer Southern Hemisphere (SH) illustrate that this event could be related to the slowdown of the Atlantic Meridional Overturning Circulation (AMOC). The comparison between the all-forcing experiment and the single-forcing experiments indicates that this event might have been caused by internal variability, while external forcings such as orbital and greenhouse gases might have modulation effects. A positive North Atlantic Oscillation (NAO)-like pattern in the atmosphere (low troposphere) triggered a negative Atlantic Multi-decadal Oscillation (AMO)-like pattern in the ocean, which then triggered a circum-global teleconnection (CGT)-like wave train pattern in the atmosphere (high troposphere). The positive NAO-like pattern and the CGT-like pattern are the direct physical processes that led to the NH cooling and mega-drought. The AMO-like pattern played a “bridge” role in maintaining this barotropic structure in the atmosphere at a multi-decadal–centennial timescale. Our work provides a global image and dynamic background to help better understand the 4.2 ka BP event.
format Article in Journal/Newspaper
author Yan, Mi
Liu, Jian
author_facet Yan, Mi
Liu, Jian
author_sort Yan, Mi
title Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
title_short Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
title_full Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
title_fullStr Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
title_full_unstemmed Physical processes of cooling and mega-drought during the 4.2 ka BP event: results from TraCE-21ka simulations
title_sort physical processes of cooling and mega-drought during the 4.2 ka bp event: results from trace-21ka simulations
publisher Copernicus Publications
publishDate 2019
url https://doi.org/10.5194/cp-15-265-2019
https://noa.gwlb.de/receive/cop_mods_00003207
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003165/cp-15-265-2019.pdf
https://cp.copernicus.org/articles/15/265/2019/cp-15-265-2019.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332
https://doi.org/10.5194/cp-15-265-2019
https://noa.gwlb.de/receive/cop_mods_00003207
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00003165/cp-15-265-2019.pdf
https://cp.copernicus.org/articles/15/265/2019/cp-15-265-2019.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/cp-15-265-2019
container_title Climate of the Past
container_volume 15
container_issue 1
container_start_page 265
op_container_end_page 277
_version_ 1766134527696044032