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Methodology ยท Gravimetry

Satellite gravimetry

Retrieves time-variable gravity-field and mass-change signals by tracking changes in distance between two co-orbiting satellites, as in GRACE and GRACE-FO.

Satellite gravimetry is the method used when the target is mass redistribution rather than surface appearance. A pair of satellites follows the same orbit; changes in the pull of Earth's gravity alter their separation, and precision inter-satellite ranging turns those distance changes into monthly gravity-field and equivalent-water-height maps. It resolves basin-to-global mass signals such as ice-sheet mass, groundwater and terrestrial water storage, and ocean-mass sea-level components. It is weak for local detail: spatial resolution is coarse, leakage corrections matter near coasts and small basins, and the retrieval depends on geophysical background corrections.

Topic
Fit
Glacier and ice-sheet massfirst choice

primary-mass-change

Groundwater and terrestrial water storagefirst choice

primary-terrestrial-water-storage

Droughtsuitable

basin-water-storage-deficit

Sea level and ocean dynamicssuitable

ocean-mass-component

Inland wateradequate

basin-total-water-storage

Snow water equivalentadequate

large-scale-snow-mass-storage

Soil moistureadequate

assimilated-regional-soil-moisture

Demonstrated
Capable, undemonstrated

None on record.

  • Determines the static gravity field and fine geoid by measuring gravity gradients directly with an onboard gradiometer, as demonstrated by GOCE.

Sources
Methodology

Edited from public sources. Last reviewed date pending by SpectraWorks editorial. See the data dictionary for field definitions.

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