2021
DOI: 10.1007/s00190-021-01488-7
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Altimeter-derived marine gravity variations reveal the magma mass motions within the subaqueous Nishinoshima volcano, Izu–Bonin Arc, Japan

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Cited by 6 publications
(4 citation statements)
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“…The Earth large-scale mass migration will cause spatiotemporal changes of the Earth gravity field (Li et al, 2021). The ocean accounts for about 71% of the global area, the determination of time-varying marine gravity field is an important research content of the Earth time-varying gravity field.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…The Earth large-scale mass migration will cause spatiotemporal changes of the Earth gravity field (Li et al, 2021). The ocean accounts for about 71% of the global area, the determination of time-varying marine gravity field is an important research content of the Earth time-varying gravity field.…”
Section: Introductionmentioning
confidence: 99%
“…Investigating the Earth time-varying gravity field mainly relies on repeated observation data of ground gravity and satellite gravity. The large-scale regional gravity field changes can be studied utilizing the multi-year gravity measurement data on the relative gravity surveying network (Liang et al, 2016). The precise gravity field changes in small areas can be investigated using repeated measurement data from absolute gravimeters on gravity stations (Greco et al, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Marine gravity anomalies are important data sources to construct Earth's gravity field, as the ocean occupies approximately 70% of the Earth's surface. High accuracy marine gravity observations are essential data for seafloor bathymetry and marine geological structure and mineral resource distributions, submarine volcanoes, and global changes (Fairhead et al, 2001;Fu et al, 2001;Smith., 2009,2014;Hwang and Chang, 2014;Li et al, 2020;Li et al, 2021).…”
Section: Introductionmentioning
confidence: 99%
“…Accordingly, the levels of accuracy and precision of altimetry-derived marine gravity field models, which can be derived from radar altimeter measurements of sea surface heights (Rapp, 1979;Haxby et al, 1983) or slopes (Sandwell and Smith, 1997;Andersen and Knudsen, 1998;Hwang, 1998), have greatly evolved. Until now, they have demonstrated accuracy and spatial resolution at 1-2 mGal and 1′ × 1′ (approximately 2 km × 2 km), respectively and, as a result, have allowed many contemporary geophysical questions to be addressed (e.g., Fairhead et al, 2001;Bao et al, 2013;Sandwell et al, 2013;Sandwell et al, 2014;Sandwell et al, 2019;Hwang and Chang, 2014;Li et al, 2020;Li et al, 2021).…”
Section: Introductionmentioning
confidence: 99%