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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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 |
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Australian National University: ANU Digital Collections |
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ftanucanberra |
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English |
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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 |
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65 |
container_issue |
18 |
container_start_page |
1505 |
op_container_end_page |
1507 |
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1788065829077647360 |