New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes

Until now, the calculation of the principal inertia moment of the triaxial three-layered Earth mainly adopts the scaling method. This method assumes that the corresponding principal inertia axes of the layers coincide each other, but this is not the case. In this paper, a rigorous tensor transformat...

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Main Authors: Wenying Zhang, Wenbin Shen
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2020-09-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984720300240
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spelling doaj-7521a0aea7dc4cae8ba68409d86976702021-04-02T09:28:58ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472020-09-01115307315New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modesWenying Zhang0Wenbin Shen1School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, ChinaSchool of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China; State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing, Wuhan University, Wuhan, 430079, China; Corresponding author. School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China.Until now, the calculation of the principal inertia moment of the triaxial three-layered Earth mainly adopts the scaling method. This method assumes that the corresponding principal inertia axes of the layers coincide each other, but this is not the case. In this paper, a rigorous tensor transformation rule is adopted to calculate the principal inertia moments (PIMs) of different layers. Appling the new estimated PIMs to the triaxial three-layered Earth rotation theory with considering various couplings, the numerical calculations show that the periods of the Chandler Wobble (CW), Free Core Nutation (FCN), Free Inner Core Nutation (FICN) and Inner Core Wobble (ICW) are respectively 433.0, 430.8, 943.9 and 2735.9 mean solar days, which are well comparable with the corresponding values accepted at present in geoscience community. Better estimates of the PIMs of different layers may provide better constrains on relevant physical parameters of the Earth's interior.http://www.sciencedirect.com/science/article/pii/S16749847203002403-D mantle density modelEarth's inertia tensorEarth rotationRotational normal modes
collection DOAJ
language English
format Article
sources DOAJ
author Wenying Zhang
Wenbin Shen
spellingShingle Wenying Zhang
Wenbin Shen
New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
Geodesy and Geodynamics
3-D mantle density model
Earth's inertia tensor
Earth rotation
Rotational normal modes
author_facet Wenying Zhang
Wenbin Shen
author_sort Wenying Zhang
title New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
title_short New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
title_full New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
title_fullStr New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
title_full_unstemmed New estimation of triaxial three-layered Earth's inertia tensor and solutions of Earth rotation normal modes
title_sort new estimation of triaxial three-layered earth's inertia tensor and solutions of earth rotation normal modes
publisher KeAi Communications Co., Ltd.
series Geodesy and Geodynamics
issn 1674-9847
publishDate 2020-09-01
description Until now, the calculation of the principal inertia moment of the triaxial three-layered Earth mainly adopts the scaling method. This method assumes that the corresponding principal inertia axes of the layers coincide each other, but this is not the case. In this paper, a rigorous tensor transformation rule is adopted to calculate the principal inertia moments (PIMs) of different layers. Appling the new estimated PIMs to the triaxial three-layered Earth rotation theory with considering various couplings, the numerical calculations show that the periods of the Chandler Wobble (CW), Free Core Nutation (FCN), Free Inner Core Nutation (FICN) and Inner Core Wobble (ICW) are respectively 433.0, 430.8, 943.9 and 2735.9 mean solar days, which are well comparable with the corresponding values accepted at present in geoscience community. Better estimates of the PIMs of different layers may provide better constrains on relevant physical parameters of the Earth's interior.
topic 3-D mantle density model
Earth's inertia tensor
Earth rotation
Rotational normal modes
url http://www.sciencedirect.com/science/article/pii/S1674984720300240
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AT wenbinshen newestimationoftriaxialthreelayeredearthsinertiatensorandsolutionsofearthrotationnormalmodes
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