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  Surface displacement, self-attraction and loading and M2 ocean tide fields in view of anelastic solid Earth models

Huang, P., Sulzbach, R., Tanaka, Y., Klemann, V., Dobslaw, H., Martinec, Z., Thomas, M. (2021): Surface displacement, self-attraction and loading and M2 ocean tide fields in view of anelastic solid Earth models.
https://doi.org/10.5880/GFZ.1.3.2021.003

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Item Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007591 Version Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5007591_1
Genre: Data Publication

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 Creators:
Huang, Pingping1, Author              
Sulzbach, Roman1, Author              
Tanaka, Yoshiyuki1, Author              
Klemann, V.1, Author              
Dobslaw, H.1, Author              
Martinec, Zdeněk2, Author
Thomas, M.1, Author              
Affiliations:
11.3 Earth System Modelling, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146027              
2External Organizations, ou_persistent22              

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Free keywords: mantle structure; analysis; sensitivity analysis; physical property; elasticity
 Abstract: As a supplement to Huang et al. (2021) “Anelasticity and lateral heterogeneities in Earth’s upper mantle: impact on surface displacements, self-attraction and loading and ocean tide dynamics”, the global amplitude and root-mean-square fields of surface vertical displacement and self-attraction and loading due to ocean tide loading - the M2 tide derived from model TiME (Sulzbach et al., 2021), and the root-mean-square fields of M2 tide are presented here. The fields have been calculated for the 1D elastic solid Earth model PREM and 3D and 1D anelastic models. Figures 4-7, S1 and S2, and tables 1-2 in Huang et al. (2021) can be easily reproduced from these data fields applying the calculus discussed in the paper. The anelastic Earth models can be constructed with the methodology outlined in Huang et al. (2021) by making use of the elastic and attenuation tomography models from the University of California, Berkeley (Karaoğlu, H. & Romanowicz, B., 2018) and the École Normale Supérieure (ENS) de Lyon (Debayle et al., 2020), respectively. All response fields (U and SAL) are calculated with the spectral-finite element method (Martinec 2000, Tanaka et al. 2019).

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Language(s): eng - English
 Dates: 20212021
 Publication Status: Finally published
 Pages: -
 Publishing info: Potsdam : GFZ Data Services
 Table of Contents: -
 Rev. Type: -
 Identifiers: DOI: 10.5880/GFZ.1.3.2021.003
GFZPOF: p4 T2 Ocean and Cryosphere
 Degree: -

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