Authors / CoAuthors
Brown, N.J. | Tregoning, P.
Abstract
The purpose of this paper is to investigate and quantify the near-field and far-field contamination effects from GRACE data to assess whether or not they influence the accuracy with which hydrological signals in the Murray-Darling Basin, southeast Australia can be estimated. Far-field contamination was assessed by modelling some of the world's largest geophysical processes which generate major gravitational signals (e.g. melting of the Greenland icesheet, hydrology in the Amazon Basin) while near-field contamination was modelled by simulating gravitational variability of the Australian continent. Contamination was measured by simulating each of the processes and measuring the proportion of the simulated signal detected in the Murray - Darling Basin. The sum of the cumulative near-field and far-field effects revealed a maximum of ~10 mm (equivalent water height) of spurious signal within the Murray - Darling Basin. This equates to only one quarter of the formal uncertainty of the basin-scale estimates of changes in total water storage. Thus, GRACE products can be used to monitor broad scale hydrologic trends and variability in the Murray-Darling Basin without the need to account for contamination of the estimates from external geophysical sources.
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nonGeographicDataset
eCat Id
69602
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Keywords
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- External PublicationScientific Journal Paper
- ( Theme )
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- groundwater
- ( Theme )
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- remote sensing
- ( Theme )
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- geodesy
- Australian and New Zealand Standard Research Classification (ANZSRC)
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- Earth Sciences
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- Published_Internal
Publication Date
2009-10-06T00:00:00
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