Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/25881
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZhang, P-
dc.creatorWai, OWH-
dc.creatorChen, X-
dc.creatorLu, J-
dc.creatorTian, L-
dc.date.accessioned2015-05-26T08:17:18Z-
dc.date.available2015-05-26T08:17:18Z-
dc.identifier.issn2073-4441-
dc.identifier.urihttp://hdl.handle.net/10397/25881-
dc.language.isoenen_US
dc.publisherMdpi Agen_US
dc.rights© 2014 by the authors; licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution license (http://creativecommons.org/licenses/by/3.0/).en_US
dc.rightsThe following publication Zhang, P., Wai, O. W. H., Chen, X., Lu, J., & Tian, L. (2014). Improving sediment transport prediction by assimilating satellite images in a tidal bay model of Hong Kong. Water (Switzerland), 6(3), (Suppl. ), 642-660 is available athttps://dx.doi.org/10.3390/w6030642en_US
dc.subjectData assimilationen_US
dc.subjectDeep bayen_US
dc.subjectMODISen_US
dc.subjectOptimal interpolationen_US
dc.subjectSatellite imageen_US
dc.subjectSediment transport modelen_US
dc.titleImproving sediment transport prediction by assimilating satellite images in a tidal bay model of Hong Kongen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage642-
dc.identifier.epage660-
dc.identifier.volume6-
dc.identifier.issue3-
dc.identifier.doi10.3390/w6030642-
dcterms.abstractNumerical models being one of the major tools for sediment dynamic studies in complex coastal waters are now benefitting from remote sensing images that are easily available for model inputs. The present study explored various methods of integrating remote sensing ocean color data into a numerical model to improve sediment transport prediction in a tide-dominated bay in Hong Kong, Deep Bay. Two sea surface sediment datasets delineated from satellite images from the Moderate Resolution Imaging Spectra-radiometer (MODIS) were assimilated into a coastal ocean model of the bay for one tidal cycle. It was found that remote sensing sediment information enhanced the sediment transport model ability by validating the model results with in situ measurements. Model results showed that root mean square errors of forecast sediment both at the surface layer and the vertical layers from the model with satellite sediment assimilation are reduced by at least 36% over the model without assimilation.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationWater (Switzerland), Mar. 2014, v. 6, no. 3, p. 642-660-
dcterms.isPartOfWater (Switzerland)-
dcterms.issued2014-
dc.identifier.isiWOS:000335896000011-
dc.identifier.scopus2-s2.0-84899802917-
dc.identifier.rosgroupidr71201-
dc.description.ros2013-2014 > Academic research: refereed > Publication in refereed journal-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_IR/PIRAen_US
dc.description.pubStatusPublisheden_US
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