Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?

Paleomagnetic records from globally distributed locations are essential for fully understanding geomagnetic field variations, particularly non-dipole field fluctuations [1]. Paleomagnetic studies on historical time scales have demonstrated the existence of persistent geomagnetic flux patches, such a...

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Published in:Science Bulletin
Main Authors: Zhong, Yi, Liu, Yanguang, Yang, Xiaoqiang, Zhang, Jian, Liu, Jiabo, Bosin, Aleksandr, Gorbarenko, Sergey A., Shi, Xuefa, Chen, Ting, Chou, Yumin, Gai, Congcong
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier B.V.
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Online Access:http://hdl.handle.net/1885/261633
https://doi.org/10.1016/j.scib.2020.05.016
https://openresearch-repository.anu.edu.au/bitstream/1885/261633/3/01_Zhong_Do_non-dipole_geomagnetic_2020.pdf.jpg
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spelling ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/261633 2024-01-14T10:10:57+01:00 Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka? Zhong, Yi Liu, Yanguang Yang, Xiaoqiang Zhang, Jian Liu, Jiabo Bosin, Aleksandr Gorbarenko, Sergey A. Shi, Xuefa Chen, Ting Chou, Yumin Gai, Congcong application/pdf http://hdl.handle.net/1885/261633 https://doi.org/10.1016/j.scib.2020.05.016 https://openresearch-repository.anu.edu.au/bitstream/1885/261633/3/01_Zhong_Do_non-dipole_geomagnetic_2020.pdf.jpg en_AU eng Elsevier B.V. 2095-9273 http://hdl.handle.net/1885/261633 doi:10.1016/j.scib.2020.05.016 https://openresearch-repository.anu.edu.au/bitstream/1885/261633/3/01_Zhong_Do_non-dipole_geomagnetic_2020.pdf.jpg © 2020 The Authors Science Bulletin Journal article ftanucanberra https://doi.org/10.1016/j.scib.2020.05.016 2023-12-15T09:33:21Z Paleomagnetic records from globally distributed locations are essential for fully understanding geomagnetic field variations, particularly non-dipole field fluctuations [1]. Paleomagnetic studies on historical time scales have demonstrated the existence of persistent geomagnetic flux patches, such as the Canadian (North America) and Siberian (East Asia) flux lobes, which may result from an organizing structure imposed on the geomagnetic field by lower mantle heterogeneity [2]. Holocene paleomagnetic secular variations, reconstructed from the Alaskan margin of the Subarctic Pacific Ocean (SPO) [3] and revealed by dynamo modeling [4], further suggest that time-varying flux expulsions on the core-mantle boundary recurrently occur in high-latitude locations (Fig. 1a). This work was supported financially by the National Natural Science Foundation of China (41874078, 41806063, and U1606401), the National Key Research & Development Program of China (2016YFA061903), National Program on Global Change and Air-Sea Interaction (GASI-GEOGE-03), the Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences (MGE2018KG05), Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao) (MGQNLM201818), SIGEPAX (03F0704A), State Key Laboratory of Marine Geology, Tongji University (MGK1826), and Shenzhen Science and Technology Program (KQTD20170810111725321). Article in Journal/Newspaper Subarctic Australian National University: ANU Digital Collections Pacific Science Bulletin 65 18 1505 1507
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language English
description Paleomagnetic records from globally distributed locations are essential for fully understanding geomagnetic field variations, particularly non-dipole field fluctuations [1]. Paleomagnetic studies on historical time scales have demonstrated the existence of persistent geomagnetic flux patches, such as the Canadian (North America) and Siberian (East Asia) flux lobes, which may result from an organizing structure imposed on the geomagnetic field by lower mantle heterogeneity [2]. Holocene paleomagnetic secular variations, reconstructed from the Alaskan margin of the Subarctic Pacific Ocean (SPO) [3] and revealed by dynamo modeling [4], further suggest that time-varying flux expulsions on the core-mantle boundary recurrently occur in high-latitude locations (Fig. 1a). This work was supported financially by the National Natural Science Foundation of China (41874078, 41806063, and U1606401), the National Key Research & Development Program of China (2016YFA061903), National Program on Global Change and Air-Sea Interaction (GASI-GEOGE-03), the Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences (MGE2018KG05), Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao) (MGQNLM201818), SIGEPAX (03F0704A), State Key Laboratory of Marine Geology, Tongji University (MGK1826), and Shenzhen Science and Technology Program (KQTD20170810111725321).
format Article in Journal/Newspaper
author Zhong, Yi
Liu, Yanguang
Yang, Xiaoqiang
Zhang, Jian
Liu, Jiabo
Bosin, Aleksandr
Gorbarenko, Sergey A.
Shi, Xuefa
Chen, Ting
Chou, Yumin
Gai, Congcong
spellingShingle Zhong, Yi
Liu, Yanguang
Yang, Xiaoqiang
Zhang, Jian
Liu, Jiabo
Bosin, Aleksandr
Gorbarenko, Sergey A.
Shi, Xuefa
Chen, Ting
Chou, Yumin
Gai, Congcong
Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
author_facet Zhong, Yi
Liu, Yanguang
Yang, Xiaoqiang
Zhang, Jian
Liu, Jiabo
Bosin, Aleksandr
Gorbarenko, Sergey A.
Shi, Xuefa
Chen, Ting
Chou, Yumin
Gai, Congcong
author_sort Zhong, Yi
title Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
title_short Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
title_full Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
title_fullStr Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
title_full_unstemmed Do non-dipole geomagnetic field behaviors persistently exist in the subarctic Pacific Ocean over the past 140 ka?
title_sort do non-dipole geomagnetic field behaviors persistently exist in the subarctic pacific ocean over the past 140 ka?
publisher Elsevier B.V.
url http://hdl.handle.net/1885/261633
https://doi.org/10.1016/j.scib.2020.05.016
https://openresearch-repository.anu.edu.au/bitstream/1885/261633/3/01_Zhong_Do_non-dipole_geomagnetic_2020.pdf.jpg
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_source Science Bulletin
op_relation 2095-9273
http://hdl.handle.net/1885/261633
doi:10.1016/j.scib.2020.05.016
https://openresearch-repository.anu.edu.au/bitstream/1885/261633/3/01_Zhong_Do_non-dipole_geomagnetic_2020.pdf.jpg
op_rights © 2020 The Authors
op_doi https://doi.org/10.1016/j.scib.2020.05.016
container_title Science Bulletin
container_volume 65
container_issue 18
container_start_page 1505
op_container_end_page 1507
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