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dc.contributor.authorKhaki, M.
dc.contributor.authorSchumacher, M.
dc.contributor.authorForootan, E.
dc.contributor.authorKuhn, Michael
dc.contributor.authorAwange, Joseph
dc.contributor.authorvan Dijk, A.
dc.date.accessioned2017-11-24T05:26:06Z
dc.date.available2017-11-24T05:26:06Z
dc.date.created2017-11-24T04:48:51Z
dc.date.issued2017
dc.identifier.citationKhaki, M. and Schumacher, M. and Forootan, E. and Kuhn, M. and Awange, J. and van Dijk, A. 2017. Accounting for spatial correlation errors in the assimilation of GRACE into hydrological models through localization. Advances in Water Resources. 108: pp. 99-112.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/58527
dc.identifier.doi10.1016/j.advwatres.2017.07.024
dc.description.abstract

© 2017 Elsevier Ltd Assimilation of terrestrial water storage (TWS) information from the Gravity Recovery And Climate Experiment (GRACE) satellite mission can provide significant improvements in hydrological modelling. However, the rather coarse spatial resolution of GRACE TWS and its spatially correlated errors pose considerable challenges for achieving realistic assimilation results. Consequently, successful data assimilation depends on rigorous modelling of the full error covariance matrix of the GRACE TWS estimates, as well as realistic error behavior for hydrological model simulations. In this study, we assess the application of local analysis (LA) to maximize the contribution of GRACE TWS in hydrological data assimilation. For this, we assimilate GRACE TWS into the World-Wide Water Resources Assessment system (W3RA) over the Australian continent while applying LA and accounting for existing spatial correlations using the full error covariance matrix. GRACE TWS data is applied with different spatial resolutions including 1° to 5° grids, as well as basin averages. The ensemble-based sequential filtering technique of the Square Root Analysis (SQRA) is applied to assimilate TWS data into W3RA. For each spatial scale, the performance of the data assimilation is assessed through comparison with independent in-situ ground water and soil moisture observations. Overall, the results demonstrate that LA is able to stabilize the inversion process (within the implementation of the SQRA filter) leading to less errors for all spatial scales considered with an average RMSE improvement of 54% (e.g., 52.23 mm down to 26.80 mm) for all the cases with respect to groundwater in-situ measurements. Validating the assimilated results with groundwater observations indicates that LA leads to 13% better (in terms of RMSE) assimilation results compared to the cases with Gaussian errors assumptions. This highlights the great potential of LA and the use of the full error covariance matrix of GRACE TWS estimates for improved data assimilation results.

dc.publisherElsevier
dc.titleAccounting for spatial correlation errors in the assimilation of GRACE into hydrological models through localization
dc.typeJournal Article
dcterms.source.volume108
dcterms.source.startPage99
dcterms.source.endPage112
dcterms.source.issn0309-1708
dcterms.source.titleAdvances in Water Resources
curtin.departmentDepartment of Spatial Sciences
curtin.accessStatusFulltext not available


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