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Global Isostatic Gravity Maps From Satellite Missions and Their Applications in the Lithospheric Structure Studies
Key Laboratory of Geospace Environment and Geodesy, Wuhan University, Wuhan, China; he New Technologies for the Information Society, University of West Bohemia, Plzen, Czech Republic.
University of Gävle, Faculty of Engineering and Sustainable Development, Department of Industrial Development, IT and Land Management, Land management, GIS. the Royal Institute of Technology, Stockholm, Sweden.
University of Trieste, Trieste, Italy.
the Royal Institute of Technology, Stockholm, Sweden.
2017 (English)In: IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, ISSN 1939-1404, E-ISSN 2151-1535, Vol. 10, no 2, 549-561 p.Article in journal (Refereed) Published
Abstract [en]

Recent satellite gravity missions provide information on the Earth’s gravity field with a global and homogenous coverage. These data have been utilized in geoscience studies to investigate the Earth’s inner structure. In this study, we use the global gravitational models to compute and compare various isostatic gravity data. In particular, we compile global maps of the isostatic gravity disturbances by applying the Airy-Heiskanen and Pratt-Hayford isostatic theories based on assuming a local compensation mechanism. We further apply the Vening Meinesz-Moritz isostatic (flexural) model based on a more realistic assumption of the regional compensation mechanism described for the Earth’s homogenous and variable crustal structure. The resulting isostatic gravity fields are used to analyze their spatial and spectral characteristics with respect to the global crustal geometry. Results reveal that each of the applied compensation model yields a distinctive spatial pattern of the isostatic gravity field with its own spectral characteristics. The Airy-Heiskanen isostatic gravity disturbances provide a very smooth gravity field with no correlation with the crustal geometry. The Pratt-Hayford isostatic gravity disturbances are spatially highly correlated with the topography on land, while the Vening-Meinesz Moritz isostatic gravity disturbances are correlated with the Moho geometry. The complete crust-stripped isostatic gravity disturbances reveal a gravitational signature of the mantle lithosphere. These general characteristics provide valuable information for selection of a particular isostatic scheme, which could be used for gravimetric interpretations, depending on a purpose of the study.

Place, publisher, year, edition, pages
2017. Vol. 10, no 2, 549-561 p.
Keyword [en]
Earth; gravity; isostasy; satellite observation systems; topography
National Category
Geophysics
Identifiers
URN: urn:nbn:se:hig:diva-24328DOI: 10.1109/JSTARS.2016.2556219ISI: 000395466700015Scopus ID: 2-s2.0-84966605787OAI: oai:DiVA.org:hig-24328DiVA: diva2:1110935
Note

Funding agencies:

National Science Foundation of China (NSFC)  grant no: 41429401 

Czech Ministry of Education, Youth and Sport by the National Program of Sustainability Grant no: LO1506 

Available from: 2017-06-16 Created: 2017-06-16 Last updated: 2017-06-16Bibliographically approved

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CiteExportLink to record
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Cite
Citation style
  • apa
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  • ieee
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  • Other style
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Language
  • sv-SE
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  • Other locale
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Output format
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