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dc.contributor.authorChappell, Adrianen_US
dc.contributor.authorMcTainsh, Granten_US
dc.contributor.authorLeys, Johnen_US
dc.contributor.authorStrong, Craigen_US
dc.date.accessioned2017-04-24T08:15:33Z
dc.date.available2017-04-24T08:15:33Z
dc.date.issued2003en_US
dc.date.modified2009-10-01T05:54:09Z
dc.identifier.issn01979337en_US
dc.identifier.doi10.1002/esp.1036en_AU
dc.identifier.urihttp://hdl.handle.net/10072/5973
dc.description.abstractThe sampling frequency in space and time is often inadequate to estimate the accuracy and precision of aeolian sediment transport. The problem stems from a lack of knowledge about the spatial and temporal scale of variation in aeolian transport and is compounded by a shortage of resources (aeolian sediment traps and labour). This study developed a geostatistical methodology for estimating sediment transport at unsampled locations and tested the extent to which it was dependent on sampling networks (nested, grid and random) and frameworks (mobile or static sampling framework between wind erosion events). Aeolian transport data were collected in an area of Australia influenced by wind erosion (Diamantina Lakes National Park, southwestern Queensland) to evaluate the combination of events used for mapping transport. Insufficient wind erosion events occurred to test sediment sampling strategies and hence simulated sampling was conducted using maps of sediment transport produced with existing models of aeolian sediment transport in the same study area. Independent validation data were used to test the estimation performance.The results suggested that sampling networks that did not include information on the spatial scale of variation (i.e. grid and random sampling) did not represent adequately the sediment transport population. In contrast, a bespoke nested sampling network performed consistently better than the other networks. Overall the static framework with a nested network was recommended for estimation and mapping of sediment transport with few resources and was likely to be especially important for use over large areas. This approach has the advantage of requiring only a single pooled within-event variogram for sediment transport to be used to derive the model parameters for kriging or stochastic simulation for each event.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherJohn Wiley and Sons Ltd.en_US
dc.publisher.placeUnited Kingdomen_US
dc.publisher.urihttp://www3.interscience.wiley.com/journal/117935722/grouphome/home.htmlen_AU
dc.relation.ispartofpagefrom1223en_US
dc.relation.ispartofpageto1241en_US
dc.relation.ispartofedition2003en_US
dc.relation.ispartofjournalEarth Surface Processes and Landformsen_US
dc.relation.ispartofvolume28en_US
dc.subject.fieldofresearchcode260114en_US
dc.titleSimulations to optimize sampling of aeolian sediment transport in space and time for mappingen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.rights.copyrightCopyright 2003 John Wiley & Sons, Ltd. Self-archiving of the author-manuscript version is not yet supported by this publisher. Please refer to the journal link for access to the definitive, published version or contact the author for more information.en_AU
gro.date.issued2003
gro.hasfulltextNo Full Text


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