Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks

Obtaining reliable reconstructions of long-term atmospheric circulation changes in the North Atlantic region presents a persistent challenge to contemporary paleoclimate research, which has been addressed by a multitude of recent studies. In order to contribute a novel methodological aspect to this...

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Main Authors: Franke, Jasper G., Werner, Johannes P., Donner, Reik V.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2017
Subjects:
550
Online Access:https://doi.org/10.34657/1224
https://oa.tib.eu/renate/handle/123456789/654
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spelling ftleibnizopen:oai:oai.leibnizopen.de:CB6CMYsBBwLIz6xG6Chm 2023-11-12T04:16:59+01:00 Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks Franke, Jasper G. Werner, Johannes P. Donner, Reik V. 2017 application/pdf https://doi.org/10.34657/1224 https://oa.tib.eu/renate/handle/123456789/654 eng eng München : European Geopyhsical Union CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ Climate of the Past, Volume 13, Issue 11, Page 1593-1608 atmospheric circulation Holocene network analysis North Atlantic Oscillation numerical model paleoclimate proxy climate record qualitative analysis reconstruction regression analysis 550 article Text 2017 ftleibnizopen https://doi.org/10.34657/1224 2023-10-15T23:19:53Z Obtaining reliable reconstructions of long-term atmospheric circulation changes in the North Atlantic region presents a persistent challenge to contemporary paleoclimate research, which has been addressed by a multitude of recent studies. In order to contribute a novel methodological aspect to this active field, we apply here evolving functional network analysis, a recently developed tool for studying temporal changes of the spatial co-variability structure of the Earth's climate system, to a set of Late Holocene paleoclimate proxy records covering the last two millennia. The emerging patterns obtained by our analysis are related to long-term changes in the dominant mode of atmospheric circulation in the region, the North Atlantic Oscillation (NAO). By comparing the time-dependent inter-regional linkage structures of the obtained functional paleoclimate network representations to a recent multi-centennial NAO reconstruction, we identify co-variability between southern Greenland, Svalbard, and Fennoscandia as being indicative of a positive NAO phase, while connections from Greenland and Fennoscandia to central Europe are more pronounced during negative NAO phases. By drawing upon this correspondence, we use some key parameters of the evolving network structure to obtain a qualitative reconstruction of the NAO long-term variability over the entire Common Era (last 2000 years) using a linear regression model trained upon the existing shorter reconstruction. publishedVersion Article in Journal/Newspaper Fennoscandia Greenland North Atlantic North Atlantic oscillation Svalbard Unknown Greenland Svalbard
institution Open Polar
collection Unknown
op_collection_id ftleibnizopen
language English
topic atmospheric circulation
Holocene
network analysis
North Atlantic Oscillation
numerical model
paleoclimate
proxy climate record
qualitative analysis
reconstruction
regression analysis
550
spellingShingle atmospheric circulation
Holocene
network analysis
North Atlantic Oscillation
numerical model
paleoclimate
proxy climate record
qualitative analysis
reconstruction
regression analysis
550
Franke, Jasper G.
Werner, Johannes P.
Donner, Reik V.
Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
topic_facet atmospheric circulation
Holocene
network analysis
North Atlantic Oscillation
numerical model
paleoclimate
proxy climate record
qualitative analysis
reconstruction
regression analysis
550
description Obtaining reliable reconstructions of long-term atmospheric circulation changes in the North Atlantic region presents a persistent challenge to contemporary paleoclimate research, which has been addressed by a multitude of recent studies. In order to contribute a novel methodological aspect to this active field, we apply here evolving functional network analysis, a recently developed tool for studying temporal changes of the spatial co-variability structure of the Earth's climate system, to a set of Late Holocene paleoclimate proxy records covering the last two millennia. The emerging patterns obtained by our analysis are related to long-term changes in the dominant mode of atmospheric circulation in the region, the North Atlantic Oscillation (NAO). By comparing the time-dependent inter-regional linkage structures of the obtained functional paleoclimate network representations to a recent multi-centennial NAO reconstruction, we identify co-variability between southern Greenland, Svalbard, and Fennoscandia as being indicative of a positive NAO phase, while connections from Greenland and Fennoscandia to central Europe are more pronounced during negative NAO phases. By drawing upon this correspondence, we use some key parameters of the evolving network structure to obtain a qualitative reconstruction of the NAO long-term variability over the entire Common Era (last 2000 years) using a linear regression model trained upon the existing shorter reconstruction. publishedVersion
format Article in Journal/Newspaper
author Franke, Jasper G.
Werner, Johannes P.
Donner, Reik V.
author_facet Franke, Jasper G.
Werner, Johannes P.
Donner, Reik V.
author_sort Franke, Jasper G.
title Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
title_short Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
title_full Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
title_fullStr Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
title_full_unstemmed Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
title_sort reconstructing late holocene north atlantic atmospheric circulation changes using functional paleoclimate networks
publisher München : European Geopyhsical Union
publishDate 2017
url https://doi.org/10.34657/1224
https://oa.tib.eu/renate/handle/123456789/654
geographic Greenland
Svalbard
geographic_facet Greenland
Svalbard
genre Fennoscandia
Greenland
North Atlantic
North Atlantic oscillation
Svalbard
genre_facet Fennoscandia
Greenland
North Atlantic
North Atlantic oscillation
Svalbard
op_source Climate of the Past, Volume 13, Issue 11, Page 1593-1608
op_rights CC BY 3.0 Unported
https://creativecommons.org/licenses/by/3.0/
op_doi https://doi.org/10.34657/1224
_version_ 1782334003124109312