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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Bibliographic Details
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.
Subjects:
Pacific
Subarctic
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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Summary: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).

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